#ONFRONTING #LIMATE #HANGE IN THE 'REAT ,AKES 2EGION )MPACTS ON /UR #OMMUNITIES AND %COSYSTEMS :+ :* >iÊ-Ì°Ê Ãi« Ê*>à «}Ê *>à -Õ«iÀÀÊ } >`à / Õ`iÀÊ>ÞÊ *>à >Ì>}> :- >iÊ-Õ«iÀÀ >«i>ÕÊ *>à ÀÌ iÀÊ>iÃÊ>`ÊÀiÃÌà «ÃÃ} > ->ÌÊ >ÕÀiÌ ÕÀ iÊ ÀÌ Ê iÌÀ>Ê >À`Ü`ÊÀiÃÌà >iÊV -ÕÌ i>ÃÌiÀÊ 7ÃVÃÊ/Ê*> }> ÕÀÌ>À Ài -ÕÌ iÀÊ V }>É ÀÌ iÀÊ `>>Ê >ÞÊ*>à i À iÊ > iÌÀ>Ê ÀÊ iÌÊ*>à >iÊ "Ì>À >ÃÌiÀÊ ÀÊ iÌÊ*>à :) 2 % 0 / 2 4 / & 4HE 5NION OF #ONCERNED 3CIENTISTS AND 4HE %COLOGICAL 3OCIETY OF !MERICA ÀiÉ"Ì>À >iÊ*> ÀÌ iÀÊ««>>V >Ê *>Ìi>ÕÊ>`Ê1«>`à ÕÀÉÀi >iÊ*> ! ÀÌ i>ÃÌiÀ } >`à #ONFRONTING #LIMATE #HANGE IN THE 'REAT ,AKES 2EGION )MPACTS ON /UR #OMMUNITIES AND %COSYSTEMS 02%0!2%$ "9 'EORGE 7 +LING +ATHARINE (AYHOE ,UCINDA " *OHNSON *OHN * -AGNUSON 3TEPHEN 0OLASKY 3COTT + 2OBINSON "RIAN * 3HUTER -ICHELLE - 7ANDER $ONALD * 7UEBBLES $ONALD 2 :AK 7)4( #/.42)"54)/.3 &2/- 2ICHARD , ,INDROTH 3USANNE # -OSER -ARK , 7ILSON !PRIL ! 2%0 /24 /& 4HE 5NION OF #ONCERNED 3CIENTISTS AND 4HE %COLOGICAL 3OCIETY OF !MERICA # / . & 2/ . 4 ) . 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' % ) . # ! , ) & / 2 . ) ! 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA #ITATION +LING '7 + (AYHOE ," *OHNSON ** -AGNUSON 3 0OLASKY 3+ 2OBINSON "* 3HUTER -- 7ANDER $* 7UEBBLES $2 :AK 2, ,INDROTH 3# -OSER AND -, 7ILSON #ONFRONTING #LIMATE #HANGE IN THE 'REAT ,AKES 2EGION )MPACTS ON OUR #OMMUNITIES AND %COSYSTEMS 5NION OF #ONCERNED 3CIENTISTS #AMBRIDGE -ASSACHUSETTS AND %COLOGICAL 3OCIETY OF !MERICA 7ASHINGTON $# Ú 5NION OF #ONCERNED 3CIENTISTS %COLOGICAL 3OCIETY OF !MERICA !LL RIGHTS RESERVED 0RINTED IN THE 5NITED 3TATES OF !MERICA $ESIGNED BY $' #OMMUNICATIONS !CTON -ASSACHUSETTS WWWNONPROlTDESIGNCOM 0RINTED ON RECYCLED PAPER #OPIES OF THIS REPORT ARE AVAILABLE FROM 5#3 0UBLICATIONS 4WO "RATTLE 3QUARE #AMBRIDGE -! n 4EL nn )N #ANADA COPIES OF THE REPORT ARE AVAILABLE FROM THE $AVID 3UZUKI &OUNDATION OR ORDERS DAVIDSUZUKIORG 4HE REPORT AND ADDITIONAL TECHNICAL BACKGROUND INFORMATION ARE ALSO AVAILABLE AT WWWUCSUSAORGGREATLAKES #OVER 0HOTO #REDITS CLOCKWISE FROM TOP RIGHT +ILLARNEY 0ROVINCIAL 0ARK /NTARIO PHOTOGRAPH BY #LAUDE 'RONDIN .IAGARA &ALLS #ENTER FOR 'REAT ,AKES AND !QUATIC 3CIENCES COURTESY OF -INN 3EA 'RANT 3LEEPING "EAR $UNES .ATIONAL ,AKESHORE -ICHIGAN PHOTOGRAPH BY 2OBERT $E*ONGE COURTESY OF -ICH 4RAVEL "UREAU AND -INN 3EA 'RANT #HICAGO )LLINOIS PHOTOGRAPH BY *OHN * -AGNUSON &ARMSCAPE NEAR #HIPPEWA &ALLS 7IS PHOTOGRAPH BY 2ON .ICHOLS COURTESY OF 53$! .ORTH 3TAR ,AKE -INN PHOTOGRAPH BY 2ICHARD &AULKNER COURTESY OF %DGE OF THE 7ILDERNESS .ATIONAL 3CENIC "YWAY II # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 4ABLE OF #ONTENTS ÛÊÊÊÊÊÊÊÊÊÊ }ÕÀià ÛÊÊÊÊÊÊÊÊ Ýià ÛÊÊÊÊÊÊÊÊ />LiÃ Û ÊÊÊÊÊÊÊ VÜi`}iiÌà £ ÊÊÊÊÊÊÊÊÊ ÝiVÕÌÛiÊ-Õ>ÀÞ Ç ÊÊÊÊÊÊÊÊÊ #HAPTER ££ )NTRODUCTION 2EGIONAL ,ANDSCAPES (UMAN 'EOGRAPHY AND %CONOMY (UMAN 0RESSURES ON %COSYSTEM (EALTH AND 3ERVICES #HAPTER 4WO -Vi>ÀÃÊvÊ >}i\Ê*>ÃÌ]Ê ÕÀÀiÌ]Ê>`ÊÕÌÕÀiÊ >Ìi Ó£ /NE Ài>ÌÊ>iÃÊVÃÞÃÌiÃÊ>`Ê*i«i\ÊÕÌÕ>ÊvÕiViÊ>`Êi«i`iVi #LIMATE 4RENDS AND 6ARIABILITY IN THE 'REAT ,AKES 2EGION (ISTORICAL 2ECORDS OF #HANGE ,AKE 4EMPERATURE )CE #OVER AND 7ATER ,EVELS 7ATER 4EMPERATURES $URATION AND %XTENT OF ,AKE )CE ,AKE 7ATER ,EVELS AND 3TREAM &LOWS 0ROJECTIONS OF &UTURE #LIMATE IN THE 'REAT ,AKES 2EGION 4EMPERATURE 0RECIPITATION %XTREME %VENTS AND 2UNOFF -IGRATING #LIMATES 4HE 0OTENTIAL FOR 3URPRISE #HAPTER 4HREE V}V>Ê6ÕiÀ>LÌÞÊÌÊ >ÌiÊ >}i\ʵÕ>ÌVÊVÃÞÃÌià ,AKE %COSYSTEMS (IGHER ,AKE 4EMPERATURES 2EDUCED )CE #OVER #HANGES IN ,AKE 7ATER ,EVELS #HANGES IN ,AKE 0RODUCTIVITY 2IVER AND 3TREAM %COSYSTEMS )MPACTS OF #HANGES IN (YDROLOGY )MPACTS OF (IGHER 7ATER 4EMPERATURE )MPACTS ON "IODIVERSITY AND &OOD 7EBS # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA III xÇ #HAPTER &OUR V}V>Ê6ÕiÀ>LÌÞÊÌÊ >ÌiÊ >}i\Ê/iÀÀiÃÌÀ>ÊVÃÞÃÌià ÈÇ &ORESTED ,ANDSCAPES $ISTRIBUTION AND 0RODUCTIVITY )MPACTS ON &OREST )NSECTS )MPACTS ON 7ILDLIFE !GRICULTURAL ,ANDSCAPES #LIMATE )MPACTS ON #ROPS )MPACTS ON !GRICULTURAL 0ESTS )MPACTS ON ,IVESTOCK %CONOMIC #ONSEQUENCES OF #LIMATE AND %COLOGICAL #HANGES IN 4ERRESTRIAL 3YSTEMS &ORESTS AND 7ILDLIFE !GRICULTURE 2ECREATION AND 4OURISM #HAPTER &IVE iiÌ}ÊÌ iÊ >i}iÃÊvÊ >ÌiÊ >}i IV 7ETLAND %COSYSTEMS )MPACTS OF #HANGES IN (YDROLOGY %COSYSTEM &UNCTIONING )MPACTS ON "IODIVERSITY &ISH 2ESPONSES TO #LIMATE #HANGE #HANGES IN &ISH $ISTRIBUTION #HANGES IN &ISH 0RODUCTIVITY %CONOMIC #ONSEQUENCES OF #LIMATE AND %COLOGICAL #HANGES IN !QUATIC 3YSTEMS 7ATER ,EVELS 3HIPPING AND (YDROPOWER 'ENERATION &ISHERIES 2EDUCING %MISSIONS BY 3ECTOR %NERGY 4RANSPORTATION 7ASTE -ANAGEMENT &ORESTRY AND !GRICULTURE )NTEGRATED %MISSION 3TRATEGIES -INIMIZING (UMAN 0RESSURES ON THE %NVIRONMENT !IR 1UALITY )MPROVEMENTS 7ATER 1UALITY 0ROTECTION AND $EMAND3UPPLY -ANAGEMENT 5RBAN AND ,AND 5SE 0LANNING (ABITAT 0ROTECTION AND 2ESTORATION # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA -ANAGING THE )MPACTS OF #LIMATE #HANGE &ISHERIES !QUATIC %COSYSTEMS 2ESOURCES AND 7ILDLIFE !GRICULTURE &ORESTRY )NFRASTRUCTURE 0ROTECTION AND "UILT %NVIRONMENTS (UMAN (EALTH -EETING THE #HALLENGES Ç ,iviÀiVià ä ÌÀLÕÌ}ÊÕÌ ÀÃ Ó -ÌiiÀ}Ê ÌÌii &IGURES &IGURE 4HE 'REAT ,AKES 2EGION &IGURE 3ATELLITE$ERIVED -APS 3HOWING ,AND #OVER AND 3OIL $RAINAGE &IGURE 0OPULATION #HANGE IN THE 'REAT ,AKES 2EGION n &IGURE 4HE 7ORLDS 4HIRD,ARGEST %CONOMY &IGURE 4HE #HANGING #HARACTER OF THE 2EGION &IGURE A /BSERVED AND 0ROJECTED #HANGE IN !VERAGE $AILY 4EMPERATURE &IGURE B /BSERVED AND 0ROJECTED #HANGE IN !VERAGE 0RECIPITATION &IGURE (ISTORICAL 4RENDS IN %XTREME 2AINFALL %VENTS n &IGURE #HANGE IN 4IMING OF ,AKE &REEZES AND 4HAWS &IGURE A )CE #OVER $URATION ON ,AKE -ENDOTA 7ISCONSIN &IGURE B +ITES ON )CE 7INTER &ESTIVAL ON ,AKE -ONONA 7ISCONSIN &IGURE 0ROJECTED #HANGES IN 4EMPERATURE $URING 3UMMER AND 7INTER BY n &IGURE 'ROWING 3EASON IN THE 'REAT ,AKES 2EGION &IGURE 0ROJECTED #HANGES IN 0RECIPITATION $URING 3UMMER AND 7INTER BY n &IGURE 3EASONAL 0RECIPITATION #YCLE &IGURE )NCREASED &REQUENCY OF (EAVY 2AINFALL %VENTS IN THE 'REAT ,AKES 2EGION &IGURE 0RECIPITATION 3HIFTS 3IGNAL 4ROUBLE FOR &ARMERS # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA V &IGURE -IGRATING #LIMATE #HANGING 7INTERS AND 3UMMERS IN )LLINOIS AND -ICHIGAN &IGURE )MPACTS ON ,AKE %COSYSTEMS &IGURE A ,AKE 3TRATIlCATION AND THE $EVELOPMENT OF h$EAD :ONESv &IGURE B ,AKE -ICHIGAN &ISH +ILL &IGURE )MPACTS ON 3TREAM %COSYSTEMS &IGURE )MPACTS ON 7ETLAND %COSYSTEMS &IGURE A 3ONGBIRD $ECLINES %XPECTED &IGURE B #LIMATE #HANGE )MPACTS ON 7ATERFOWL &IGURE ,EOPARD &ROG IN 7ISCONSIN 7ETLAND &IGURE 4EMPERATURE 'ROUPINGS OF #OMMON 'REAT ,AKES &ISH &IGURE 7ATER 4EMPERATURE AND &ISH $ISTRIBUTION #HANGES &IGURE 7ATER #HANGES !FFECT (YDROPOWER &IGURE 4HE .ORTHERN &ORESTS &IGURE A &OREST 0ESTS IN A #HANGING #LIMATE &IGURE B 'YPSY -OTH ,ARVA &EEDING ON !SPEN ,EAF &IGURE 2ANGE 3HIFTS OF THE #ANADIAN 4IGER 3WALLOWTAIL &IGURE 6IRGINIA 0OSSUMS 2ANGE %XPANDING .ORTH &IGURE -IXED )MPACTS FOR !GRICULTURE &IGURE #LIMATE #HANGE AND !GRICULTURAL 0ESTS &IGURE A 4EMPERATURE %XTREMES IN THE 'REAT ,AKES 2EGION &IGURE B #ONCERNS !BOUT )NSECTBORNE )NFECTIOUS $ISEASES &IGURE #LIMATE #HANGE )MPACTS ON THE 4IMBER )NDUSTRY &IGURE )MPACTS ON 3UMMER 2ECREATION &IGURE -INNESOTA 7IND &ARM &IGURE )LLINOIS &UEL #ELL "US &IGURE A 4ORONTOS h'REENv #ITY (ALL &IGURE B #APTURING -ETHANE 'AS FROM ,ANDlLL &IGURE &IGURE A %COLOGICAL ,IMITS TO !DAPTATION IN !GRICULTURE )LLINOIS 3OIL &IGURE B .ORTHERN -ICHIGAN 3OIL &IGURE VI -INIMIZING 3PRAWL -ANAGING THE ,AKE AND 3TREAM )MPACTS OF #LIMATE #HANGE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA "OXES 4HE )NTERNATIONAL #ONSENSUS ON #LIMATE #HANGE .ATURAL 6ARIABILITY ,ONG4ERM #HANGES AND THE #HALLENGE OF 0REDICTION /N 4HIN )CE IN -ADISON #LIMATE #HANGE AND h$EAD :ONESv IN ,AKE %RIE #LIMATE AND "IRD $IVERSITY ON -ICHIGANS 5PPER 0ENINSULA %XTREME %VENTS 0UBLIC (EALTH AND THE (UMAN %NVIRONMENT (OW #ONlDENT #AN 7E "E !BOUT #LIMATE #HANGE )MPACTS ON 'REAT ,AKES %COSYSTEMS 4ORONTO ! ,EADER !MONG #ITIES IN 2EDUCING 'REENHOUSE 'AS %MISSIONS 4ABLES 4ABLE )CE #OVER %XPECTED TO $ECREASE IN THE 'REAT ,AKES 2EGION 4ABLE 7ATER ,EVELS ,IKELY TO $ECREASE IN THE &UTURE AS SHOWN HERE FOR THE 'REAT ,AKES #RYSTAL ,AKE 7ISCONSIN AND GROUNDWATER NEAR ,ANSING -ICHIGAN 4ABLE %XPECTED %FFECTS OF 7ARMER AND $RIER 3UMMER #LIMATE ON ,AKES AND 3UBSEQUENT )MPACTS ON !LGAL 0RODUCTIVITY 4ABLE )MPACTS OF #LIMATE #HANGE ON 3TREAM %COSYSTEMS 4ABLE )MPACTS OF #LIMATE #HANGE ON 7ETLAND %COSYSTEMS 4ABLE #HANGES /BSERVED 0REDICTED AND 0OSSIBLE IN THE 2ANGES OF &ISH 3PECIES IN THE ,AKES AND 2IVERS OF THE 'REAT ,AKES "ASIN 4ABLE #LIMATE #HANGE )MPACTS ON &ISH %COLOGY AND #ONSEQUENCES FOR &ISHERIES 4ABLE 4OTAL 'REENHOUSE 'AS %MISSIONS BY 3TATE0ROVINCE AND 3ECTOR 4ABLE %XAMPLES OF !DAPTIVE -EASURES FOR -ITIGATING )MPACTS OF #LIMATE #HANGE ON &ISHERIES # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA VII !CKNOWLEDGEMENTS 4HE AUTHORS THANK THE STEERING COMMITTEE OF THIS PROJECT AND ESPECIALLY ,OUIS 0ITELKA FOR CONCEPTUAL GUIDANCE AND REVIEW OF THE REPORT -ARY "ARBER PAST HER CALL OF DUTY AT %3! AND 0ETER &RUMHOFF FROM 5#3 PROVIDED LEADERSHIP FROM THE TWO SPONSORING ORGANIZATIONS )N ADDITION WE APPRECIATE THE MORE THAN TWODOZEN INDIVIDUALS WHO PROVIDED SCIENTIlC PEER REVIEW OF ALL OR PORTIONS OF EARLIER VERSIONS OF THIS REPORT /UR SINCERE THANKS FOR ENSUR ING SCIENTIlC ACCURACY GO TO $AVID !LLAN "ENNET "RABSON !LEX "OSTON 3COTT "RIDGHAM 1UENTIN #HIOTTI 0ETER #URTIS %VAN $ELUCIA +IERAN $ONAGHY ,AURIE $RINKWATER 'ABE &ILIPPELLI !NN . &ISHER 0IERRE 'OSSELIN $AVE 'RIGAL 'LENN 'UNTENSPERGEN $ANNY (ARVEY "OB (ECKY *OAN +LAASSEN 4IM +RATZ 5RIEL $ +ITRON ! #ARL ,EOPOLD 3ARAH -ARCHILDON 0AM -ATSON 0ATRICK * -ULHOLLAND ,E2OY 0OFF 4ERRY 2OOT )AN 2UTHERFORD 'ERRY 3COTT +RISTIN 3HRADER&RECHETTE "RENT 3OHNGEN AND 3COTT 3WINTON !NY REMAIN ING ERRORS ARE OURS OF COURSE -ANY INDIVIDUALS ALSO SUPPLIED DATA TECHNICAL INFORMATION AND COPIES OF PUBLISHED OR FORTHCOMING RESEARCH PAPERS 4HANK YOU TO 2ICHARD !DAMS 6ICTOR " #ABALLERO 3TEVE #LEMMER *EFF $EYETTE 'LENN 'UNTENSPERGEN +SHAMA (ARPANKAR 4OM (OLLENHORST 4IM *OHNSON -ICHELLE -ANION !LAN .OGEE *OHN 0ASTOR *EFF 0RICE !ARON 2APPAPORT (AROLD 2ENNIE 0HIL 2YAN 0AUL 3TRODE .ORI 4ARUI AND -ICHAEL 7ARD )N ADDITION +ENNETH +UNKEL SUPPLIED HISTORICAL CLIMATE DATA AND CONTRIBUTED TO THE CLIMATE CHAPTER $AVID 6INER PROVIDED ACCESS TO (AD#- MODEL RESULTS AND -ICHAEL 7EHNER AND *ERRY -EEHL PROVIDED ACCESS TO 0#- MODEL RESULTS (ELP IN IDENTIFYING PRODUCING AND SUPPLYING GRAPHICS AND PHOTOGRAPHS CAME FROM !LEX "OSTON 4ARYN #LARK 4IM $ANIEL 2OBERT $ARMODY #LAUDE 'RONDIN 3VENJA (ANSEN $AVE (ANSON *AMES - (AYNES 4OM (OLLENHORST ,INDA (OLTHAUS $AVE (VIZDAK ,UCINDA *OHNSON 4IM *OHNSON $ENISE +ARNS 'EORGE +LING -ARTY +ROELL 2OBERT -C,EESE *OHN * -AGNUSON 3ARAH -ARCHILDON 2ON -OEN *OHN 0ASTOR *ULIA 0ETIPAS -ARIE 2EYNOLDS ,ARRY 2ICKER +EITH 3TEWART 0AUL 3TRODE $AVID 4AYLOR 3COTT ! 4HOM -ICHAEL 7ARD -IKE 7ILLIAMS (EATHER 7EBB AND -INNESOTA 3EA 'RANT 6ANESSA 0ARKER'EISMAN HELPED TREMENDOUSLY WITH lNDING AND CHOOSING BETWEEN GRAPHICS AND KEPT TRACK OF THEM ALL 4HE PRODUCTION OF THIS REPORT WAS MADE POSSIBLE THROUGH THE GENEROUS SUPPORT OF 4HE (ENRY ,UCE &OUNDATION )NC WITH ADDITIONAL FOUNDATION SUPPORT FROM THE *OHN $ AND #ATHERINE 4 -AC!RTHUR &OUNDATION -ARBROOK &OUNDATION /AK &OUNDATION THE 6 +ANN 2ASMUSSEN &OUNDATION AND 7ALLACE 'LOBAL &UND 4HE 5NIVERSITY OF )LLINOIS /FlCE OF THE 6ICE #HANCELLOR FOR 2ESEARCH AND THE )LLINOIS)NDIANA 3EA 'RANT 0ROGRAM /FlCE lNANCIALLY SUPPORTED THE CLIMATE MODELING WORK 4HE $AVID 3UZUKI &OUNDATION 6ANCOUVER "RITISH #OLUMBIA GENEROUSLY PROVIDED FUNDING FOR SOME WORK RELATED TO THE #ANADIAN PORTION OF THE PROJECT 4HE REPORT WILL BE RELEASED UNDER THE AUSPICES OF THE $3& IN /NTARIO &INALLY WE COULD NOT HAVE COMPLETED THIS PROJECT WITHOUT 2HONDA +RANZ OF THE %COLOGICAL 3OCIETY OF !MERICA AND 3USANNE -OSER OF THE 5NION OF #ONCERNED 3CIENTISTS WHO PERSISTENTLY AND PATIENTLY MANAGED THE PROJECT THROUGH ITS DIFFERENT PHASES VIII # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA %XECUTIVE 3UMMARY 4 HE 'REAT ,AKES REGION OF THE 5NITED 3TATES AND #ANADA IS A LAND OF STRIKING GLACIAL LEGACIES SPECTACULAR LAKES VAST WETLANDS FERTILE SOUTHERN SOILS AND RUGGED NORTHERN TERRAIN FORESTED IN SPRUCE AND FIR )T IS ALSO HOME TO MILLION PEOPLE WHOSE ACTIONS CAN PROFOUNDLY AFFECT THE REGIONS ECOLOGICAL BOUNTY AND THE LIFESUSTAINING BENEFITS IT PROVIDES .OW THAT THE WORLD IS ENTERING A PERIOD OF UNUSUALLY RAPID CLIMATE CHANGE DRIVEN LARGELY BY HUMAN ACTIVITIES THAT RELEASE HEATTRAPPING GREENHOUSE GASES INTO THE ATMOSPHERE THE RESPONSIBILITY FOR SAFEGUARDING OUR NATURAL HERITAGE IS BECOMING URGENT 'ROWING EVIDENCE SUGGESTS THAT THE CLIMATE OF THE 'REAT ,AKES REGION IS ALREADY CHANGING % 7INTERS ARE GETTING SHORTER % !NNUAL AVERAGE TEMPERATURES ARE GROWING WARMER % 4HE DURATION OF LAKE ICE COVER IS DECREASING AS AIR AND WATER TEMPERATURES RISE % (EAVY RAINSTORMS ARE BECOMING MORE COMMON 4HIS REPORT EXAMINES THESE TRENDS IN DETAIL AND DISCUSSES THE LIKELIHOOD THAT THEY WILL CONTINUE INTO THE FUTURE 4HE CONSEQUENCES OF THESE CLIMATIC CHANGES WILL MAGNIFY THE IMPACTS OF ONGOING HUMAN DISTURBANCES THAT FRAGMENT OR TRANSFORM LANDSCAPES POLLUTE AIR AND WATER AND DISRUPT NATURAL ECOSYSTEMS AND THE VITAL GOODS AND SERVICES THEY PROVIDE #ONFRONTING #LIMATE #HANGE IN THE 'REAT ,AKES 2EGION EXPLORES THE POTENTIAL CONSEQUENCES OF CLIMATE CHANGE GOOD AND BAD FOR THE CHARACTER ECONOMY AND ENVIRONMENT OF THE 'REAT ,AKES REGION DURING THE COMING CENTURY )T ALSO EXAMINES ACTIONS THAT CAN BE TAKEN NOW TO HELP FORESTALL MANY OF THE MOST SEVERE CONSEQUENCES OF CLIMATE CHANGE FOR .ORTH !MERICAS HEARTLAND # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA %XECUTIVE 3UMMARY ÊÊÊÊÊÊÊÊÊÊÊÊ7 >ÌÊÃÊÌ iÊ iÞÊV>ÌiÊvÕÌÕÀiÊvÀÊ ÊÊÊÊÊÊÌ iÊÀi>ÌÊ>iÃÊÀi}¶ )N GENERAL THE CLIMATE OF THE 'REAT ,AKES REGION WILL GROW WARMER AND PROBABLY DRIER DURING THE TWENTY FIRST CENTURY #LIMATE MODELS PREDICT THAT BY THE END OF THE CENTURY TEMPERATURE IN THE REGION WILL WARM BY TO & TO # IN WINTER AND BY TO & TO # IN SUMMER .IGHTTIME TEMPERATURES ARE LIKELY TO WARM MORE THAN DAYTIME TEMPERATURES AND EXTREME HEAT WILL BE MORE COMMON !NNUAL AVERAGE PRECIPITATION LEVELS ARE UNLIKELY TO CHANGE BUT THE SEASONAL DISTRIBUTION IS LIKELY TO VARY GREATLY INCREAS ING IN WINTER AND DECREASING IN SUMMER /VERALL THE REGION MAY GROW DRIER BECAUSE ANY INCREASES IN RAIN OR SNOW ARE UNLIKELY TO COMPENSATE FOR THE DRYING EFFECTS OF INCREASED EVAPORATION AND TRANSPIRATION IN A WARMER CLIMATE 4HIS DRYING WILL AFFECT SURFACE AND GROUNDWATER LEVELS AND SOIL MOISTURE IS PROJECTED TO DECREASE BY PERCENT IN SUMMER )N ADDITION THE FREQUENCY OF HOUR AND MULTIDAY DOWNPOURS AND THUS FLOODING MAY CONTINUE TO INCREASE 4HESE CHANGES IN TEMPERATURE AND PRECIPITATION WILL STRONGLY ALTER HOW THE CLIMATE FEELS TO US 7ITHIN THREE DECADES FOR EXAMPLE A SUMMER IN )LLINOIS MAY FEEL LIKE A SUMMER IN /KLAHOMA DOES TODAY "Y THE END OF THE CENTURY AN )LLINOIS SUMMER MAY WELL FEEL LIKE ONE IN EAST 4EXAS TODAY WHILE A -ICHIGAN SUM MER WILL PROBABLY FEEL LIKE AN !RKANSAS SUMMER DOES TODAY 2ESIDENTS IN 4ORONTO COULD EXPERIENCE A SHIFT FROM A SOUTHERN /NTARIO SUMMER TO ONE THAT BY MAY FEEL MORE LIKE ONE IN UPSTATE .EW 9ORK AND BY THE END OF THE CENTURY MORE LIKE ONE IN NORTHERN 6IRGINIA TODAY ÊÊÊÊÊÊÊÊÊÊÊÊ7 >ÌÊ} ÌÊÌ iÃiÊ V >}iÃÊi>ÊvÀÊÀi>ÌÊ>iÃÊ ÊÊÊÊÊÊÊÊiVÃÞÃÌiÃÊ>`ÊÌ iÊ}`ÃÊ ÊÊÊÊÊ>`ÊÃiÀÛViÃÊÌ iÞÊ«ÀÛ`i¶Ê >ià s ,AKE LEVELS HAVE BEEN HIGHLY VARIABLE IN THE S BUT DECLINES IN BOTH THE INLAND LAKES AND THE 'REAT ,AKES ARE ANTICIPATED IN THE FUTURE s $ECLINES IN THE DURATION OF WINTER ICE ARE EXPECTED TO CONTINUE s ,OSS OF WINTER ICE MAY BE A MIXED BLESSING FOR FISH REDUCING WINTERKILL IN SHALLOW LAKES BUT ALSO JEOPAR DIZING REPRODUCTION OF WHITEFISH IN THE 'REAT ,AKES BAYS WHERE ICE COVER PROTECTS THE EGGS FROM WINTER STORM DISTURBANCE s 4HE DISTRIBUTIONS OF MANY FISH AND OTHER ORGANISMS IN LAKES AND STREAMS WILL CHANGE #OLDWATER SPECIES SUCH AS LAKE TROUT BROOK TROUT AND WHITEFISH AND COOLWATER SPECIES SUCH AS NORTHERN PIKE AND WALLEYE ARE LIKELY TO DECLINE IN THE SOUTHERN PARTS OF THE REGION WHILE WARMWATER SPECIES SUCH AS SMALLMOUTH BASS AND BLUEGILL ARE LIKELY TO EXPAND NORTHWARD s )NVASIONS BY NATIVE SPECIES CURRENTLY FOUND JUST TO THE SOUTH OF THE REGION AND INVASIONS OF WARM WATER NONNATIVE SPECIES SUCH AS COMMON CARP WILL BE MORE LIKELY INCREASING THE STRESS ON NATIVE PLANT AND ANIMAL POPULATIONS IN THE REGION s )N ALL LAKES THE DURATION OF SUMMER STRATIFICATION WILL INCREASE ADDING TO THE RISK OF OXYGEN DEPLE TION AND FORMATION OF DEEPWATER hDEAD ZONESv FOR FISH AND OTHER ORGANISMS # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA s ,OWER WATER LEVELS COUPLED WITH WARMER WATER TEMPERATURES MAY ACCELERATE THE ACCUMULATION OF MERCURY AND OTHER CONTAMINANTS IN THE AQUATIC FOOD CHAIN AND ULTIMATELY IN FISH s -ANY FISH SPECIES SHOULD GROW FASTER IN WARMER WATERS BUT TO DO SO THEY MUST INCREASE THEIR FEEDING RATES )T REMAINS UNCERTAIN WHETHER PREY SPECIES AND THE FOOD WEB RESOURCES ON WHICH THEY DEPEND WILL INCREASE TO MEET THESE NEW DEMANDS -ÌÀi>ÃÊ>`Ê7iÌ>`à s %ARLIER ICE BREAKUP AND EARLIER PEAKS IN SPRING RUNOFF WILL CHANGE THE TIMING OF STREAM FLOWS AND INCREASES IN HEAVY RAINSTORMS MAY CAUSE MORE FREQUENT FLOODING s #HANGES IN THE TIMING AND SEVERITY OF FLOOD PULSES ARE LIKELY TO REDUCE SAFE BREEDING SITES ESPECIALLY FOR AMPHIBIANS MIGRATORY SHOREBIRDS AND WATERFOWL AND MAY CAUSE MANY NORTHERN MIGRATORY SPECIES SUCH AS #ANADA GEESE TO WINTER FURTHER NORTH s ,AND USE CHANGE AND HABITAT FRAGMENTATION COMBINED WITH CLIMATE CHANGEINDUCED SHRINK ING OF STREAMS AND WETLANDS WILL ALSO DECREASE THE NUMBER AND TYPE OF REFUGIA AVAILABLE TO AQUATIC ORGANISMS ESPECIALLY THOSE WITH LIMITED DISPERSAL CAPABILITIES SUCH AS AMPHIBIANS AND MOLLUSKS AS STREAMS AND WETLANDS SHRINK ÀiÃÌà s 4HE DISTRIBUTION OF FORESTS IS LIKELY TO CHANGE AS WARMER TEMPERATURES CAUSE THE EXTENT OF BOREAL FORESTS TO SHRINK AND MANY FOREST SPECIES TO MOVE NORTHWARD 4HE NEW FOREST COMPOSITION WILL DEPEND ON THE ABILITY OF INDIVIDUAL SPECIES TO COLONIZE NEW SITES AND THE PRESENCE OF BOTH GEOGRAPHIC AND HUMAN BARRIERS TO MIGRATION s )NCREASING ATMOSPHERIC #/ CON CENTRATION IS LIKELY TO SPUR FOREST GROWTH IN THE SHORT TERM BUT THE `i«iÌÊ>`Ê LONGTERM RESPONSE IS NOT CLEAR AT `ii«Ü>ÌiÀʺ`i>`Ê PRESENT )NCREASING GROUNDLEVEL OZONE CONCENTRATIONS FOR EXAMPLE âiûÊÜÊVÀi>ÃiÊ WILL PROBABLY DAMAGE FOREST TREES Ê>Ê>ið POTENTIALLY OFFSETTING THE POSITIVE s 2EDUCED SUMMER WATER LEVELS ARE EFFECT OF #/ LIKELY TO DIMINISH THE RECHARGE OF GROUNDWATER s #ONTINUED DEPOSITION OF NITROGEN FROM THE SUPPLIES CAUSE SMALL STREAMS TO DRY UP AND REDUCE ATMOSPHERE MAY SPUR GROWTH IN FORESTS BUT THE THE AREA OF WETLANDS RESULTING IN POORER WATER LONGTERM CONSEQUENCES INCLUDE INCREASED NITRATE QUALITY AND LESS HABITAT FOR WILDLIFE POLLUTION OF WATERWAYS GROUNDWATER AND DRINK s $ROUGHT AND LOWER WATER LEVELS MAY ULTIMATELY ING WATER SUPPLIES INCREASE ULTRAVIOLET RADIATION DAMAGE TO FROGS AND s ,ONGDISTANCE MIGRATORY BIRDS SUCH AS SCARLET TAN OTHER AQUATIC ORGANISMS ESPECIALLY IN CLEAR AGERS WARBLERS THRUSHES AND FLYCATCHERS DEPEND SHALLOW WATER BODIES ON TREES AND CATERPILLARS FOR FOOD %SPECIALLY FOR s 2IVER FLOODING MAY BECOME MORE COMMON AND THOSE MIGRANTS WHO TIME THEIR MIGRATION BY DAY EXTREME BECAUSE OF THE INTERACTION OF MORE FREQUENT LENGTH RATHER THAN BY WEATHER FOOD SOURCES MAY RAINSTORMS WITH URBANIZATION AND OTHER LAND MAN BE SEVERELY REDUCED WHEN THEY ARRIVE IN THE 'REAT AGEMENT PRACTICES THAT INCREASE PAVEMENT AND ,AKES REGION OTHER IMPERVIOUS SURFACES AND DEGRADE THE NATURAL s 2ESIDENT BIRDS SUCH AS NORTHERN CARDINALS CHICKA FLOODABSORBING CAPACITIES OF WETLANDS AND FLOOD DEES AND TITMICE MIGHT BE ABLE TO BEGIN BREEDING PLAINS 4HE RESULT COULD BE INCREASED EROSION EARLIER AND RAISE MORE BROODS EACH SEASON (OW ADDITIONAL WATER POLLUTION FROM NUTRIENTS PESTI EVER INCREASING POPULATIONS OF RESIDENT SPECIES CIDES AND OTHER CONTAMINANTS AND POTENTIAL COULD FURTHER REDUCE THE FOOD AVAILABLE FOR MIGRA DELAYS IN RECOVERY FROM ACID RAIN TORY SONGBIRDS THAT BREED IN THE 'REAT ,AKES ULTIMATELY REDUCING FOREST BIRD DIVERSITY IN THE REGION / iÊÀÃÊvÊÝÞ}iÊ # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA %XECUTIVE 3UMMARY s 4HE GEOGRAPHIC RANGE OF FOREST PEST SPECIES SUCH AS THE GYPSY MOTH IS LIKELY TO EXPAND AS TEMPERATURES WARM AND THE DISTRIBUTION OF FOOD PLANTS CHANGES s #HANGES IN LEAF CHEMISTRY DUE TO #/ FERTILIZATION ARE POSSIBLE REDUCING FOOD QUALITY FOR SOME ORGAN ISMS 4HIS COULD CAUSE SOME LEAFEATING PESTS TO EAT MORE AND COULD ULTIMATELY ALTER AQUATIC AND TERRESTRIAL FOOD WEBS s 7ARMER TEMPERATURES MAY IMPAIR LIVESTOCK HEALTH IN SOUTHERN PARTS OF THE REGION AND A DRIER SUMMER CLIMATE MAY REDUCE THE PRODUCTIVITY OF PASTURE GRASSES s /VERALL THE INFLUENCE OF CLIMATE CHANGE ON BOTH CROP AND LIVESTOCK SECTORS WILL BE GREATLY MODERATED BY TECHNOLOGICAL ADVANCES AND TRENDS IN MARKETS (OWEVER INCREASING VARIABILITY IN THE CLIMATE IS LIKELY TO INCREASE ECONOMIC RISKS FOR SMALLER FARMS }ÀVÕÌÕÀi s %ARLIER STUDIES PREDICTED THAT CLIMATE CHANGE WOULD VV]Ê-V>]Ê>`Êi>Ì Ê«>VÌÃÊ BENEFIT OR ONLY MARGINALLY DISRUPT 'REAT ,AKES s !S LAKE LEVELS DROP COSTS TO SHIPPING IN THE 'REAT AGRICULTURAL PRODUCTIVITY OVER THE NEXT YEARS ,AKES ARE LIKELY TO INCREASE ALONG WITH COSTS OF WITH WARMING AND INCREASED #/ FERTILIZATION DREDGING HARBORS AND CHANNELS AND OF ADJUSTING BOOSTING YIELDS IN THE NORTHERN PARTS OF THE REGION DOCKS WATER INTAKE PIPES AND OTHER INFRASTRUCTURE .EWER CLIMATE PROJECTIONS USED IN THIS REPORT /N THE OTHER HAND A LONGER ICEFREE SEASON WILL HOWEVER SUGGEST A LESS FAVORABLE IMPACT ON AGRI INCREASE THE SHIPPING SEASON CULTURE LARGELY BECAUSE OF CHANGES IN THE DISTRIBU s 3HORTER WARMER WINTERS WILL RESULT IN LOSSES IN TION OF RAIN 7ETTER PERIODS ARE EXPECTED DURING WINTER RECREATION SUCH AS SKIING ICE FISHING AND TIMES THAT COULD DELAY HAR SNOWMOBILING BUT MAY LENGTHEN VEST OR PLANTING AND DRY THE SEASON FOR WARMWEATHER REC ÜiÀÊÃÕiÀÊÜ>ÌiÀÊiÛiÃÊ SPELLS ARE PROJECTED DURING REATION #HANGES IN RECREATIONAL TIMES WHEN CROPS NEED WA >ÀiÊiÞÊÌÊ`à ÊÌ iÊ FISHING HUNTING AND WILDLIFE VIEW TER !S OPTIMAL AGRICULTURAL ING MAY OCCUR AS THE DISTRIBUTION ÀiV >À}iÊvÊ}ÀÕ`Ü>ÌiÀ]Ê CLIMATES MOVE NORTHWARD OF SPECIES SHIFTS ACROSS THE REGION AND EASTWARD CROP YIELDS V>ÕÃiÊÃ>ÊÃÌÀi>ÃÊÌÊ`ÀÞÊ MAY BE LIMITED BY SOIL QUAL s #LIMATE WARMING MAY LOWER Õ«]Ê>`ÊÀi`ÕViÊÌ iÊ>Ài>Ê ITY AND BE MORE VULNERABLE HEATING COSTS IN WINTER BUT THAT TO WEATHER EXTREMES SUCH AS MAY BE OFFSET BY HIGHER COSTS FOR vÊÜiÌ>`ð FLOODS AND DROUGHTS AIR CONDITIONING IN SUMMER s 4HE LENGTH OF THE GROWING SEASON WILL CONTINUE TO INCREASE SO THAT BY THE END OF THE CENTURY IT MAY BE FOUR TO NINE WEEKS LONGER THAN OVER THE PERIOD n s #ROP LOSSES MAY INCREASE AS NEW PESTS AND DISEASES BECOME ESTABLISHED IN THE REGION AND AS WARMER LONGER GROWING SEASONS FACILITATE THE BUILDUP OF LARGER PEST POPULATIONS !LREADY THE RANGE OF THE BEAN LEAF BEETLE A PEST OF SOYBEANS APPEARS TO BE SHIFTING NORTHWARD s /ZONE CONCENTRATIONS ALREADY REACH LEVELS THAT DAMAGE SOYBEANS AND HORTICULTURAL CROPS AND INCREASING CONCENTRATIONS MAY COUNTERACT THE INCREASED PRODUCTION EXPECTED FROM #/ FERTILIZATION s 7ATER WITHDRAWALS FROM THE 'REAT ,AKES ARE ALREADY THE SUBJECT OF CONTENTIOUS DEBATE AND PRESSURES FOR MORE WATER FOR IRRIGATION DRINKING AND OTHER HUMAN USES MAY INTENSIFY THE CONFLICTS AS WATER SHORTAGES DEVELOP s $ECREASED WATER LEVELS COULD REDUCE HYDROPOWER GENERATION IN THE REGION s -ORE DAYS WITH HIGH HEAT MAY EXACERBATE THE FORMATION OF DANGEROUS LEVELS OF OZONE /ZONE AND OTHER AIR POLLUTANTS GENERATED BY COALFIRED POWER PLANTS IN THE REGION ARE LIKELY TO EXACER BATE ASTHMA AND OTHER RESPIRATORY DISEASES s (EALTH RISKS ASSOCIATED WITH EXTREME HEAT ARE LIKELY TO INCREASE WHILE COLDRELATED ILLNESSES ARE LIKELY TO DECREASE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA ÊÊÊÊÊÊÜÊV>ÊÀiÃ`iÌÃÊvÊ Ì iÊÀi>ÌÊ>iÃÊÀi}Ê>``ÀiÃÃÊÌ iÊÊÊÊÊÊÊÊÊÊÊÊÊÊ Ì iÊÀi>ÌÊ>iÃÊÀi}Ê>``ÀiÃÃÊÌ iÊÊÊÊÊÊÊÊÊÊÊÊ ÊÊÊÊÊÊÊÊV >i}iÊvÊ>ÊV >}}ÊV>Ìi¶ 4HERE ARE PRUDENT AND RESPONSIBLE ACTIONS THAT CITI ZENS AND POLICYMAKERS CAN TAKE NOW TO REDUCE THE VULNERABILITY OF ECOSYSTEMS AND SAFEGUARD THE ECONO MY OF THE REGION IN THE FACE OF A CHANGING CLIMATE 4HESE ACTIONS REPRESENT THREE COMPLEMENTARY APPROACHES AS WELL AS AQUATIC HABITATS REDUCING URBAN SPRAWL AND ATTENDANT HABITAT DESTRUCTION AND FRAGMENTA TION RESTORING CRITICAL HABITATS AND PREVENTING THE SPREAD OF INVASIVE NONNATIVE SPECIES s !NTICIPATING AND PLANNING FOR THE IMPACTS OF CHANGE TO REDUCE FUTURE DAMAGE 4HIS MAY INCLUDE / iÀiÊ>ÀiÊ«ÀÕ`iÌÊ>`Ê A WIDE RANGE OF ADAPTATIONS ÀiëÃLiÊ>VÌÃÊÌ >ÌÊVÌâiÃÊ FROM SHIFTS IN FISHERIES MAN >`Ê«VÞ>iÀÃÊV>ÊÌ>iÊÜÊ AGEMENT AND FARMING ACTIVI TIES TO CHANGES IN BUILDING ÌÊÀi`ÕViÊÌ iÊÛÕiÀ>LÌÞÊvÊ CODES AND PUBLIC HEALTH MAN AGEMENT PLANS TO PREPARE FOR iVÃÞÃÌiÃÊ>`ÊÃ>vi}Õ>À`ÊÌ iÊ EXTREME WEATHER EVENTS s 2EDUCING THE REGIONS CON TRIBUTION TO THE GLOBAL PROBLEM OF HEATTRAPPING GREENHOUSE GAS EMISSIONS !LTHOUGH SOME WARMING IS INEVITABLE AS A RESULT OF HISTORICAL EMISSIONS OF #/ MANY OF THE MOST iVÞÊvÊÌ iÊÀi}° DAMAGING IMPACTS CAN BE AVOIDED IF THE PACE AND #LIMATE CHANGE IS ALREADY EVENTUAL SEVERITY OF CLIMATE CHANGE ARE MODERATED MAKING AN IMPACT ON THE ENVIRONMENT OF THE 'REAT 3TRATEGIES FOR REDUCING EMISSIONS INCLUDE INCREASING ,AKES REGION 7AITING TO BEGIN REDUCING EMISSIONS ENERGY EFFICIENCY AND CONSERVATION IN INDUSTRIES OR TO PLAN FOR MANAGING THE EFFECTS OF CLIMATE CHANGE AND HOMES BOOSTING THE USE OF RENEWABLE ENERGY ONLY INCREASES THE EVENTUAL EXPENSE AND THE POTENTIAL SOURCES SUCH AS WIND POWER IMPROVING VEHICLE FUEL FOR IRREVERSIBLE LOSSES &ORTUNATELY MANY OF THE ACTIONS EFFICIENCY REDUCING THE NUMBER OF MILES DRIVEN THAT CAN BE TAKEN NOW TO PREVENT THE MOST DAMAGING AVOIDING WASTE AND RECYCLING IMPACTS OF CLIMATE CHANGE CAN ALSO PROVIDE IMMEDI ATE COLLATERAL BENEFITS SUCH AS COST SAVINGS CLEANER AIR s -INIMIZING HUMAN PRESSURES ON THE GLOBAL AND AND WATER IMPROVED HABITAT AND RECREATIONAL OPPOR LOCAL ENVIRONMENT TO REDUCE THE VULNERABILITY OF TUNITIES AND ENHANCED QUALITY OF LIFE IN COMMUNITIES ECOSYSTEMS AND VITAL ECOLOGICAL SERVICES TO CLIMATE THROUGHOUT THE REGION CHANGE 0RUDENT ACTIONS INCLUDE REDUCING AIR POL LUTION PROTECTING THE QUALITY OF WATER SUPPLIES # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 'REAT L AKES %COSYSTEMS AND 0EOPLE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA #(!04%2 /NE 'REAT ,AKES %COSYSTEMS AND 0EOPLE -UTUAL )NFLUENCE AND $EPENDENCE 4 HE UNIQUE WATERS AND LANDFORMS OF THE INCREASED BY MORE THAN $& $# GROWING SEASONS 'REAT ,AKES REGION ARE A STRIKING LEGACY HAVE LENGTHENED AND PRECIPITATION HAS INCREASED BY OF CLIMATES PAST &OR TWO AND A HALF MIL TO PERCENT SINCE /THER INDICATORS THAT THE LION YEARS MASSIVE ICE SHEETS ADVANCED CLIMATE IS WARMING INCLUDE DOCUMENTED LOSSES IN THE AND RETREATED ACROSS THE LAND SCOURING THE BEDROCK EXTENT OF ALPINE GLACIERS SEA ICE AND SEASONAL SNOW GOUGING OUT SPECTACULAR LAKE BASINS AND DEPOSIT COVER ING THE GEOLOGICAL FORERUNNERS OF THE SOILS THAT NOW %VIDENCE STRONGLY SUGGESTS THAT CURRENT CLIMATE NURTURE FORESTS FARMS AND GARDENS 4HE ECOSYSTEMS CHANGE IS BEING DRIVEN BY INCREASING ATMOSPHERIC CON AND HUMAN ECONOMIES OF THE REGION LIKE THE LAND CENTRATIONS OF GREENHOUSE GASES MAINLY CARBON DIOXIDE SCAPE ITSELF HAVE BEEN PROFOUNDLY SHAPED BY THIS #/ BUT ALSO METHANE #( AND NITROUS OXIDE CLIMATIC LEGACY .OW THE WORLD IS ./ 4HE MAIN REASON FOR THE ENTERING ANOTHER PERIOD OF CLIMATE BUILDUP OF THESE GASES IS THE BURNING / iÊÛ>ÃÌÊ>ÀÌÞÊ CHANGE THIS TIME UNUSUALLY RAPID AND OF FOSSIL FUELS THE CLEARING OF FORESTS vÊÃViÌÃÌÃÊ>ÀiÊ DRIVEN LARGELY BY HUMAN ACTIVITIES THAT AND OTHER ACTIVITIES OF A BURGEONING RELEASE HEATTRAPPING GREENHOUSE GASES HUMAN POPULATION 7ITHOUT MAJOR ÜÊViÀÌ>ÊÌ >ÌÊ INTO THE ATMOSPHERE 4HE IMPACTS OF SHIFTS IN GLOBAL POLICIES OR ENERGY TECH Ì iÊÜÀ`½ÃÊV>ÌiÊ THIS CLIMATE CHANGE IN CONCERT WITH NOLOGIES THESE CHANGES IN THE ATMO OTHER HUMAN PRESSURES ON OUR LANDS SPHERE WILL CONTINUE %VEN IF HUMAN ÃÊV >}}° AND WATERS PROMISE TO ALTER THE EMISSIONS WERE TO BE REDUCED DRAS CHARACTER ECONOMY AND ENVIRONMENT TICALLY #/ ALREADY IN THE ATMO OF THE 'REAT ,AKES REGION DURING THE TWENTYlRST SPHERE WOULD TAKE DECADES TO DECAY ENSURING CONTINU CENTURY %XAMINING THE POTENTIAL IMPACTS OF FUTURE ING IMPACTS ON THE CLIMATE FOR SEVERAL GENERATIONS CLIMATE ON THE REGION IS THE PURPOSE OF THIS REPORT ,IFE ON EARTH HAS RARELY EXPERIENCED SHIFTS IN CLIMATE 4HE VAST MAJORITY OF SCIENTISTS ARE NOW CERTAIN AS RAPID AS THOSE NOW IN PROGRESS AND IT IS UNCLEAR THAT THE WORLDS CLIMATE IS CHANGING !VERAGE GLOBAL WHETHER THE PLANTS ANIMALS AND ECOSYSTEMS ON WHICH TEMPERATURES ARE WARMING AND THE CURRENT RATE HUMANS DEPEND CAN ADAPT QUICKLY ENOUGH 4HESE EXCEEDS THE NORMAL RANGE OF TEMPERATURE SWINGS FACTORS LEND ADDED URGENCY TO THE NEED TO ADDRESS EXPERIENCED FOR AT LEAST THE LAST THOUSAND YEARS BOTH THE CAUSES AND THE IMPACTS OF CLIMATE CHANGE 4EMPERATURES IN THE NORTHERN HEMISPHERE HAVE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 'REAT L AKES %COSYSTEMS AND 0EOPLE ,i}>Ê>`ÃV>«iÃÊ 4 HE 'REAT ,AKES BASIN ENCOMPASSES MORE THAN SQUARE MILES OF THE .ORTH !MERICAN HEARTLAND AND CONTAINS THE LARGEST SINGLE CON CENTRATION OF LIQUID FRESH 1,Ê£ / iÊÀi>ÌÊ>iÃÊ,i} WATER ON THE PLANET 4HE lVE 'REAT ,AKES THEM SELVES COVER MORE THAN SQUARE MILES AND HOLD ABOUT PERCENT OF THE WORLDS SUPPLY OF FRESH WATER 4HE REGION HOSTS NOT ONLY THE LARGEST LAKE IN THE WORLD ,AKE 3UPERIOR AND THE FOUR OTHER 'REAT ,AKES %RIE (URON -ICHIGAN -iiÊ«>}iÊÎÎ AND /NTARIO BUT ALSO vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi HUNDREDS OF THOUSANDS OF SMALLER LAKES STREAMS AND 1,ÊÓ WETLANDS ±THE GREATEST ->ÌiÌiiÀÛi`Ê>«ÃÊ- Ü}Ê >`Ê ÛiÀÊ>`Ê-ÊÀ>>}i CONCENTRATION OF SMALL WATER BODIES IN THE WORLD IN AN AREA OF THIS SIZE &IGURE 4HIS REPORT FOCUSES ON THE SIX 'REAT ,AKES STATES )LLINOIS )NDIANA -iiÊ«>}iÊÎÎ -ICHIGAN -INNESOTA vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi /HIO AND 7ISCONSIN THE SOUTHERN HALF OF THE PROVINCE OF /NTARIO AND PORTIONS OF .EW 9ORK AND 0ENNSYLVANIA WITHIN THE BOUNDARIES OF THE 'REAT ,AKES "ASIN &IGURE "ECAUSE OF THE WAY ECONOMIC AND SOCIAL STATISTICS ARE COLLECTED THIS REPORT WILL SOMETIMES TALK ABOUT THE SIX 'REAT ,AKES STATES PLUS /NTARIO 4HE GLACIAL HISTORY OF THE REGION CONSTRAINS AND INmUENCES MOST ASPECTS OF THE ENVIRONMENT 4HE REPEATED GLACIATIONS THAT BEGAN MILLION YEARS AGO ENDED WITH THE LAST ICE AGE WHICH COVERED THE ENTIRE REGION AS FAR SOUTH AS THE /HIO 2IVER FROM TO YEARS AGO 4HE ICE lNALLY RECEDED COMPLETELY ABOUT YEARS AGO LEAVING THE MARK OF ITS PASSING ON THE CURRENT LANDSCAPE #URRENT PATTERNS OF LAND COVER AND LAND USE IN THE REGION &IGURE MIRROR THE DISTRIBUTION OF SOILS AND SEDIMENTS LEFT BY THE GLACIERS )N THE NORTHERN UPLAND REGION LOCATED ON THE #ANADIAN 3HIELD THIN COARSETEXTURED SOILS SUP PORT EXTENSIVE SPRUCE AND lR FORESTS 4HE COLD CLIMATE AND RELATIVELY POOR SOILS HAVE DISCOURAGED DEVELOP MENT OF LARGE POPULATION CENTERS AND THE ECONOMY DEPENDS LARGELY ON TOURISM TIMBER AND MINING )N THE LOWLAND AREAS TO THE SOUTH AND EAST DEEP AND FERTILE SOILS COMBINED WITH A WARMER CLIMATE SUP PORT A LARGE PROPORTION OF THE AGRICULTURAL PRODUCTION FOR BOTH #ANADA AND THE 5NITED 3TATES ALONG WITH REMNANT OAK AND HICKORY FORESTS AND PRAIRIE HABITAT Õ>Êi}À>« ÞÊ>`ÊVÞ - ORE THAN MILLION PEOPLE LIVE IN THE 'REAT ,AKES STATES AND /NTARIO HALF OF THEM WITHIN THE 'REAT ,AKES DRAINAGE BASIN ITSELF AND THE POPULATION CONTINUES TO GROW 0OPULATION GREW BY PERCENT IN THE 'REAT ,AKES STATES OVER THE PAST DECADE &IGURE AND PERCENT OVER THE SAME PERIOD IN /NTARIO -ANY MAJOR CITIES ARE SITUATED ON THE SHORES OF THE 'REAT ,AKES INCLUDING "UFFALO #HICAGO #LEVELAND $ETROIT (AMILTON -ILWAUKEE 4ORONTO AND 7INDSOR 4HE ECONOMY OF THE REGION IS LARGE AND DIVERSIlED AND INCLUDES STRONG MANUFACTURING SERVICES INCLUD ING TOURISM AND RECREATION AGRICULTURE FORESTRY AND GOVERNMENT SECTORS &IGURE 2EGIONAL PRODUCTION IN TOTALED NEARLY TRILLION 53 AN AMOUNT THAT EXCEEDS THE GROSS DOMESTIC PRODUCTION OF ANY NATION EXCEPT THE 5NITED 3TATES AND *APAN 4HE 'REAT ,AKES REGION FORMS THE INDUSTRIAL HEART LAND OF .ORTH !MERICA )N OVER PERCENT OF THE VALUE OF MANUFACTURING SHIPMENTS IN #ANADA CAME FROM /NTARIO AND THE SIX 'REAT ,AKES STATES CONTRIBUTE MORE THAN PERCENT OF TOTAL VALUE ADDED 4HE TERM GENERALLY MEANS THE ENHANCED VALUE OF A COMMODITY WHEN PROCESSED INTO A SECONDARY MORE VALUABLE PRODUCT OR SERVICE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA IN 53 MANUFACTURING %ARLY INDUSTRY RELIED UPON RAW MATERIALS MINED OR HARVESTED IN THE REGION AND LOWCOST SHIPPING ON THE LAKES )RON ORE FROM NORTH ERN -INNESOTA FOR INSTANCE WAS SHIPPED DOWN THE LAKES TO FEED THE GIANT STEEL MILLS OF 'ARY AND 0ITTS BURGH )N RECENT YEARS THE ECONOMY HAS BECOME MORE DIVERSIlED AND NO LONGER RELIES TO SUCH A LARGE DEGREE ON STEEL AUTOMOBILE MANUFACTURING AND OTHER HEAVY INDUSTRY 4HE REGION REMAINS A MAJOR SHIPPING CENTER HOWEVER AND FREIGHTERS PLY THE LAKES AND SEA WAY CORRIDORS TO THE !TLANTIC /CEAN CARRYING GRAIN SOYBEANS COAL IRON ORE AND OTHER GOODS AND COM MODITIES WORTH BILLIONS OF DOLLARS FROM THE -IDWEST AND #ANADA TO MARKETS WORLDWIDE 4HIS TRAFlC GEN ERATES BILLION 53 IN YEARLY BUSINESS REVENUE AND JOBS 4HE REGION ALSO FORMS PART OF THE AGRICULTURAL HEARTLAND OF THE CONTINENT AND MORE THAN PERCENT OF THE TOTAL VALUE OF 53 AGRICULTURAL PRODUCTS IS GROWN IN THE 'REAT ,AKES STATES 4HAT INCLUDES MORE THAN PERCENT OF THE NATIONS CORN AND PERCENT OF ITS SOYBEANS !GRICULTURAL HARVESTS ON THE #ANADIAN SIDE OF THE BASIN REPRESENT NEARLY PERCENT OF THAT NATIONS OUTPUT AND TOTAL FARM CASH RECEIPTS IN /NTARIO EXCEED THOSE FROM ALL OTHER PROVINCES IN #ANADA EXCEPT !LBERTA !LTHOUGH FORESTRY CONTRIBUTES LESS TO THE REGIONAL ECONOMY THAN INDUSTRY OR AGRICULTURE LOCALLY IMPOR TANT FORESTRY SECTORS REMAIN &OR EXAMPLE THE FOREST PRODUCTS INDUSTRY IN /NTARIO EMPLOYED MORE THAN PEOPLE AND GENERATED RECEIPTS OF MORE THAN BILLION #DN IN THE LATE S )N 7ISCONSIN IN PULP PAPER WOOD PRODUCTS MANUFACTURING AND OTHER FOREST PRODUCTS INDUSTRIES EMPLOYED WORKERS AND GENERATED MORE THAN BILLION 53 IN SHIPMENTS 4HE SERVICES SECTOR WHICH INCLUDES MANY TOURISM RECREATION AND ENVI 1 , Ê Î *«Õ>ÌÊ >}iÊÊÌ iÊ RONMENTRELATED ENTER Ài>ÌÊ>iÃÊ,i}Ê­£xäqÓä䣮 PRISES HAS GROWN IN CREASINGLY IMPORTANT AND IS NOW ONE OF THE LARGEST ECONOMIC SECTORS IN THE REGION 4HE 'REAT ,AKES THEMSELVES REPRESENT THE MAJOR RECREATION AND TOURISM ATTRACTION IN MIDDLE !MERICA )NDI ANA $UNES .ATIONAL ,AKESHORE AND 3LEEPING -iiÊ«>}iÊÎ{ "EAR $UNES .ATIONAL vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi ,AKESHORE IN -ICHIGAN EACH HOSTED MORE THAN 1 , Ê { ONE MILLION VISITORS IN / iÊ7À`½ÃÊ/ À`>À}iÃÌÊVÞÊ ­ÊÃÊvÊ1-Ê>Àî )N /NTARIO PARKS FROM 0OINT 0ELEE TO ,AKE 3UPERIOR DREW MORE THAN MILLION VISITORS ALTOGETHER )N ADDITION CROWDS OF SUMMER VACA TIONERS mOCK TO THE MANY SMALL INLAND LAKES OF .ORTHERN -ICHIGAN -INNESOTA /NTARIO AND 7ISCONSIN )N WINTER TOO LARGE NUMBERS OF -iiÊ«>}iÊÎ{ vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi VISITORS ARRIVE TO TAKE ADVANTAGE OF OPPORTUNITIES FOR DOWNHILL AND CROSS COUNTRY SKIING AND SNOWMOBILING -ORE THAN MILLION PEOPLE IN THE 'REAT ,AKES STATES PARTICIPATE IN lSHING HUNTING OR WILDLIFE WATCHING &IGURE ACTIVITIES THAT BRING BILLION 53 IN SALES ANNUALLY )N /NTARIO TRAVEL AND TOURISM BROUGHT IN MORE THAN BILLION #DN IN Õ>Ê*ÀiÃÃÕÀiÃÊÊVÃÞÃÌiÊi>Ì Ê>`Ê-iÀÛVià 4 HE WELLBEING OF PEOPLE IN THE 'REAT ,AKES REGION DEPENDS ON THE HEALTHY FUNCTIONING OF ECOSYSTEMS AND THE SERVICES THEY PROVIDE 3OME OF THESE SERVICES ARE EASILY VALUED BECAUSE THEY ARE BOUGHT SOLD OR TRADED #LEARLY AGRICULTURE FOR ESTRY TOURISM AND OUTDOOR RECREATION RELY DIRECTLY ON THE VITALITY OF BOTH NATURAL AND MANAGED ECO SYSTEMS AND THE PLANT AND ANIMAL COMMUNITIES THEY HARBOR /THER ECOLOGICAL PROCESSES HAVE NOT BEEN ASSIGNED ANY DIRECT ECONOMIC VALUE YET THEY SUPPLY VITAL SUPPORT SERVICES SUCH AS AIR AND WATER PURIlCA TION mOOD PROTECTION PEST CONTROL SOIL RENEWAL # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 'REAT L AKES %COSYSTEMS AND 0EOPLE HABITAT AESTHETIC VALUES AND SUPPORT OF CULTURAL TRADI PERCENT FROM NATURAL GAS AND PERCENT FROM COAL TIONS ESPECIALLY FOR .ATIVE !MERICANS AND &IRST .ATIONS 4HE PACE OF LANDUSE CHANGE IS LIKELY TO CONTINUE GROUPS &OREST BIRDS AND AMPHIBIANS FOR EXAMPLE TO OUTSTRIP POPULATION GROWTH IN THE REGION THANKS TO SERVE HUMANS BY DEVOURING INSECTS THAT WOULD OTHER URBAN SPRAWL AND VACATION HOME DEVELOPMENT &ROM 1,Êx WISE HARM PEOPLE FORESTS TO THE POPULATION OF NORTHEASTERN )LLINOIS / iÊ >}}Ê >À>VÌiÀÊvÊÌ iÊ,i} AND CROPS !MPHIBIANS GREW BY ONLY PERCENT WHILE RESIDENTIAL LAND CON MAY BE ESPECIALLY IMPOR SUMPTION INCREASED BY NEARLY PERCENT )N -ICHI TANT AS CONSUMERS OF GAN THE POPULATION IS PROJECTED TO GROW PERCENT MOSQUITOES IN SMALL BETWEEN AND BUT URBANIZED LAND MAY EPHEMERAL WETLANDS INCREASE TO PERCENT DURING THAT PERIOD )N /N THAT LACK lSH TARIO THE GREATER 4ORONTO AREA IS EXPECTED TO EXPAND 4HESE AND OTHER ITS URBANIZED AREA BY PERCENT BY THE YEAR ECOLOGICAL SERVICES AND -UCH OF THE LAND NOT TAKEN UP BY URBAN SPRAWL IS THE ECOSYSTEMS AND SPE GIVEN TO AGRICULTURE AND ALMOST HALF OF THE LAND IN CIES THAT SUPPLY THEM THE 'REAT ,AKES STATES HAS BEEN CONVERTED TO CROP FACE INCREASING PRESSURE lELDS PASTURES AND DAIRY FARMS -iiÊ«>}iÊÎ{ NOT ONLY FROM HUMAN #ONVERTING LAND FROM FOREST OR GRASSLAND TO FARMS vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi INDUCED CLIMATE CHANGES HOUSES SHOPPING MALLS OR FACTORIES NOT ONLY RESULTS BUT FROM MANY DIRECT HUMAN DISTURBANCES AS WELL IN OUTRIGHT LOSS OF HABITAT FOR PLANT AND ANIMAL SPECIES 4HESE INCLUDE LAND DEVELOPMENT AND LANDUSE CHANGE BUT ALSO FRAGMENTS THE LANDSCAPE LEAVING ISLANDS OF DISCHARGES OF POLLUTANTS INTO THE AIR AND WATER TIMBER NATURAL HABITAT ISOLATED IN A SEA OF HUMAN DEVELOP HARVESTING MINING INTENSIVE AGRICULTURE TOURISM MENT 4HESE HABITAT REMNANTS MAY BE TOO SMALL AND AND EVEN SHIPPING AN ACTIVITY RESPONSIBLE FOR INTRO DEGRADED TO SUSTAIN HEALTHY PLANT AND ANIMAL POPULA DUCING THE ZEBRA MUSSEL AND OTHER DAMAGING NON TIONS ESPECIALLY WHEN ROADS FENCES AND OTHER HUMAN NATIVE INVASIVE SPECIES INTO THE 'REAT ,AKES !S THE STRUCTURES CREATE BARRIERS TO MIGRATION BETWEEN THEM POPULATION OF THE REGION GROWS THESE DIRECT STRESSES ,ANDSCAPE FRAGMENTATION ALSO MAKES IT MORE DIFlCULT WILL INCREASE SO TOO WILL THE REGIONS CONTRIBUTION TO FOR SPECIES TO MIGRATE TO SUITABLE NEW HABITATS AS THE CHANGES IN THE ATMOSPHERE AND INDIRECTLY CLIMATE CLIMATE SHIFTS 4HE SIX 'REAT ,AKES STATES USE AN ESTIMATED 5RBAN DEVELOPMENT GREATLY MODIlES LOCAL HYDROL QUADRILLION "45S 0* OF ENERGY EACH YEAR OGY AS WELL BY INCREASING THE EXTENT OF IMPERVIOUS SUR /F THIS TOTAL MORE THAN FACES SUCH AS ROOFS AND PAVE PERCENT COMES FROM BURNING MENT AND DESTROYING NATURAL V}V>ÊÃiÀÛViÃÊ>`ÊÌ iÊiV FOSSIL FUELS PERCENT FROM WETLANDS AND mOODPLAINS THAT PETROLEUM PERCENT FROM ÃÞÃÌiÃÊ>`ÊëiViÃÊÌ >ÌÊÃÕ««ÞÊ WOULD OTHERWISE ABSORB STORM COAL AND PERCENT FROM NATU RUNOFF AND RECHARGE GROUND Ì iÊv>ViÊVÀi>Ã}Ê«ÀiÃÃÕÀiÊ RAL GAS %LECTRICITY PRODUCTION WATERS )NCREASING IMPER IN THIS PART OF THE 5NITED 3TATES vÀÊV>ÌiÊV >}iÊ>`ÊÌ iÀÊ VIOUS SURFACES IN A WATERSHED DEPENDS HEAVILY ON BURNING BY TO PERCENT CAUSES A Õ>Ê`ÃÌÕÀL>Við COAL WHICH EMITS THE MOST TO PERCENT INCREASE IN CARBON PER "45 -ORE THAN SURFACE RUNOFF 0AVED SUR PERCENT OF ELECTRICITY IN THE SIX STATES IS GENERATED FACES ALSO BEHAVE AS HEAT SINKS RAISING AIR AND STREAM BY COALlRED POWER PLANTS )N CONTRAST TO THE 53 WATER TEMPERATURES 2EMOVING STREAMBANK TREES STATES IN THE REGION /NTARIO ELECTRICITY PRODUCTION EXACERBATES THIS HEATING /VERALL THE IMPACTS OF IS HIGHLY DIVERSIlED WITH PERCENT FROM COAL AND CLIMATE CHANGE ON THE ENVIRONMENT AND ON HUMAN NATURAL GAS &OR ITS TOTAL ENERGY NEEDS /NTARIO CUR WELLBEING IN THE 'REAT ,AKES REGION WILL BE STRONGLY RENTLY USES 0* QUADRILLION "45S PER YEAR MODIlED BY CHANGES IN POPULATION URBANIZATION INCLUDING PERCENT FROM PETROLEUM PRODUCTS LAND USE AND POLICY AND MANAGEMENT DECISIONS # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA #(!04%2 4W O 3CENARIOS OF #HANGE 0AST #URRENT AND &UTURE #LIMATE 4 WO MAJOR FACTORS THAT SHAPE THE REGIONS GAIN AND LOSE HEAT MORE SLOWLY THAN THE SURROUNDING CLIMATE ARE ITS LOCATION IN THE MIDDLE OF LAND SURFACE WATER TEMPERATURES IN THE LAKES TEND TO THE .ORTH !MERICAN LAND MASS AND THE BE WARMER THAN THE LAND DURING THE LATE FALL AND EARLY PRESENCE OF THE 'REAT ,AKES 4HE MIDCON WINTER #ONVERSELY LAKE WATER REMAINS MUCH COLDER TINENT MIDLATITUDES LOCATION FAR FROM THE OCEANS CON THAN THE SURROUNDING LAND IN THE LATE SPRING AND TRIBUTES TO LARGE SEASONAL SWINGS IN AIR TEMPERATURE SUMMER 4HIS PHENOMENON MODERATES AIR TEMPERA BETWEEN WARM SUMMERS AND COLD WINTERS )N THE TURES NEAR THE SHORES OF THE LAKES 4HE INmUENCE OF WINTER BITTERLY COLD !RCTIC AIR THE LAKES IS MOST EVIDENT ON THE MASSES OCCASIONALLY MOVE SOUTH / iÊÀi>ÌÊ>iÃÊÌ iÃiÛiÃÊ ÊÊ DOWNWIND SIDES WHERE IT HELPS WARD INTO THE REGION AND THE TO CREATE MICROCLIMATES SUCH i«ÊVÀi>ÌiÊÕµÕiÊV>ÌVÊ POLAR JET STREAM IS OFTEN LOCATED AS THE WINEGROWING REGIONS NEAR OR OVER THE REGION 4HE OF SOUTHWESTERN -ICHIGAN AND vi>ÌÕÀiÃ]ÊÃÕV Ê>ÃÊ>iivviVÌÊ RESULT IS FREQUENT STORM SYSTEMS /NTARIO 0ERHAPS THE BESTKNOWN ÃÜv>ÃÊ>`ÊVÀV>ÌiÃÊ ASPECT OF THE 'REAT ,AKES INmU THAT BRING CLOUDY WINDY CONDITIONS AND RAIN OR SNOW )N ENCE DOWNWIND HOWEVER IS LiivV>ÊvÀÊÜiÊ}ÀÜ}° THE SUMMER A SEMIPERMANENT hLAKEEFFECTv SNOWFALL $URING HIGHPRESSURE SYSTEM IN THE THE LATE FALL AND WINTER COLD SUBTROPICAL !TLANTIC PUMPS WARM HUMID AIR INTO THE AIR MASSES SWEEP ACROSS THE WARMER LAKES PICKING REGION PARTICULARLY THE SOUTHERN PORTIONS OF THE UP HEAT AND MOISTURE AND GENERATING EXTREME SNOW 'REAT ,AKES BASIN STORMS ON THE LEE SIDES OF THE LAKES ! LAKEEFFECT 4HE 'REAT ,AKES THEMSELVES HAVE A SUBSTANTIAL SNOWSTORM IN DUMPED SEVEN FEET OF SNOW IMPACT ON THE CLIMATE "ECAUSE LARGE BODIES OF WATER IN "UFFALO OVER SEVERAL DAYS >ÌiÊ/Ài`ÃÊ>`Ê6>À>LÌÞÊÊÌ iÊÀi>ÌÊ>iÃÊ,i} . ATURAL VARIATIONS IN CLIMATE ARE DRIVEN BY MANY FACTORS INCLUDING CHANGES IN SOLAR RADIATION REACHING THE %ARTH THE DIRECTION AND INTENSITY OF OCEAN CURRENTS THAT GENERATE %L .I®O AND ,A .I®A EVENTS NATURAL mUCTUATIONS IN GREEN HOUSE GASES SUCH AS WATER VAPOR #/ AND OZONE AND CHAOTIC INTERACTIONS WITHIN THE EARTHCLIMATE SYSTEM 4HE STATE OF THE SCIENCE ON CURRENTLY OBSERVED CLIMATE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . 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FEW EPISODES OF EXTREME COLD OCCURRED IN THE S BUT MOST YEARS SAW A LESSENING OF COLD WAVES s 4HE LAST SPRING FREEZE HAS BEEN OCCURRING PROGRES SIVELY EARLIER AND CURRENT DATES ARE APPROXIMATELY ONE WEEK EARLIER THAN AT THE BEGINNING OF THE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . 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' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 3CENARIOS OF #HANGE ÃÌÀV>Ê,iVÀ`ÃÊvÊ >}i\Ê >iÊ/i«iÀ>ÌÕÀi]ÊViÊ ÛiÀ]Ê>`Ê7>ÌiÀÊiÛià " ECAUSE THE 'REAT ,AKES ARE CRITICALLY IMPORTANT TO THE REGIONAL ECONOMY EXCELLENT RECORDS HAVE BEEN KEPT OF VARIATIONS IN THEIR WATER TEMPERATURE ICE COVER AND WATER LEVELS 4HESE LONG TERM RECORDS HELP IN IDENTIFYING TRENDS THAT MAY EXTEND INTO OR BE AMPLIlED IN THE FUTURE 1,ÊÇ 7>ÌiÀÊ/i«iÀ>ÌÕÀià 4HE KEY TRENDS OBSERVED FROM WATER TEMPERATURE RECORDS OF THE 'REAT ,AKES AND OTHER INLAND LAKES INCLUDE ÃÌÀV>Ê/Ài`ÃÊÊÝÌÀiiÊ ,>v>ÊÛiÌÃÊ­£Î£q£È® -iiÊ«>}iÊÎx vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi 1,Ên >}iÊÊ/}ÊvÊ>iÊ ÀiiâiÃÊ>`Ê/ >Üà -iiÊ«>}iÊÎx vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi s )NCREASES IN NEAR SHORE WATER TEMPERATURES AT FIVE OF SEVEN SITES IN THE EASTERN 'REAT ,AKES AREA HAVE LENGTHENED THE PERIOD OF SUMMER STRATIFICATION OF THE LAKES BY ONE TO SIX DAYS PER DECADE 3TRATIFICA TION IS THE LAYERING AND SEPARATION OF WARMER SURFACE WATERS FROM COOLER BOTTOM WATERS A PHENOMENON THAT PREVENTS TURNOVER AND OXYGENATION OF BOTTOM WATERS s )NCREASINGLY WARMER WATER TEMPERATURES HAVE BEEN OBSERVED IN SPRING AND FALL OVER THE LAST YEARS AND SUMMER WATER TEMPERATURES HAVE ALSO INCREASED THOUGH LESS DRAMATICALLY s ,OCAL TRENDS IN WATER TEMPERATURE COR RELATE WITH TRENDS IN GLOBAL MEAN AIR TEMPER ATURE SUGGESTING THAT CLIMATE CHANGES IN THE 'REAT ,AKES MAY TRACK CHANGES IN GLOBAL TEMPERATURE ÕÀ>ÌÊ>`ÊÝÌiÌÊvÊ>iÊVi 3HIFTS IN THE DURATION AND EXTENT OF ICE COVER ON LAKES AND STREAMS ARE HIGHLY SENSITIVE INDICATORS OF CLIMATE VARIABILITY AND CHANGE 4HUS THEY CAN PROVIDE EARLY SIGNS OF ECOSYSTEM RESPONSES TO CLIMATE CHANGE #ONSISTENT HISTORICAL CHANGES IN ICE COVER HAVE BEEN OBSERVED IN THE INLAND LAKES AND IN THE BAYS OF THE 'REAT ,AKES THEMSELVES s &REEZEUP HAS BEEN OCCURRING LATER IN FALL AND ICEOUT THE LOSS OF ICE COVER IN SPRING EARLIER IN SPRING FOR THE PAST CENTURY &IGURE AND THE RATES OF CHANGE HAVE BEEN GREATER IN THE PAST YEARS THAN OVER THE PRECEDING YEARS 2ECENTLY THE FALL FREEZE HAS BEEN MOVING LATER BY DAYS PER DECADE AND SPRING BREAKUP EARLIER BY DAYS PER DECADE s 2ECORDS OVER THE PAST TO YEARS CONSISTENT LY SHOW SHORTER PERIODS OF ICE COVER SEE BOX P s #HANGES IN ICE COVER FOR THE INLAND LAKES ARE GREATEST IN -ICHIGAN -INNESOTA AND 7ISCONSIN &IGURE )N .EW 9ORK AND /NTARIO LAKEEFFECT SNOWFALL CAN DELAY ICE BREAKUP ALTHOUGH IT DOES NOT INFLUENCE THE FALL FREEZE DATE )N THE 'REAT ,AKES THEMSELVES THE EXTENT OF ICE COVER HAS BEEN HIGHLY VARIABLE FROM TO THE PRESENT WITH NO LONGTERM TREND HOWEVER IN RECENT YEARS THE 'REAT ,AKES HAVE HAD LITTLE ICE COVER s /CCURRENCES OF UNUSUALLY EXTENSIVE ICE COVER HAVE DECLINED IN RECENT YEARS WHILE PERIODS OF GREATLY REDUCED OR NO ICE COVER HAVE BECOME MORE FRE QUENT )N THE WINTER OF FOR EXAMPLE A NUMBER OF INLAND .EW 9ORK LAKES WITH A HISTORY OF ICE COVER DID NOT FREEZE s 9EARTOYEAR VARIATIONS IN ICE COVER ARE ASSOCIATED IN PART WITH LARGESCALE CLIMATE DRIVERS SUCH AS %L .I®O THE .ORTH !TLANTIC /SCILLATION AND THE STRENGTH OF THE !LEUTIAN LOW 4HESE DRIVERS CAN IN TURN BE INFLUENCED BY THE BUILDUP OF HEATTRAPPING # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 3CENARIOS OF #HANGE GREENHOUSE GASES 2ECENT ANALYSES SUGGEST THAT %L .I®OS ARE BECOMING STRONGER AND THE INFLUENCE OF %L .I®OS ON EARLIER ICE BREAKUP HAS INCREASED IN RECENT YEARS 3HIFTS IN ICE COVER NOT ONLY SIGNAL A RESPONSE TO CLIMATE CHANGE BUT ALSO DRIVE FURTHER ECOLOGICAL SOCIAL AND CLIMATE IMPACTS 2EDUCED ICE COVER LEADS TO GREATER EVAPORATION FROM OPEN WATER IN WINTER WHICH CONTRIBUTES TO LOWER WATER LEVELS LOSS OF WINTER RECREATION ON LAKES AND PERHAPS AN INCREASE IN LAKE EFFECT SNOWS DEPENDING ON AIR TEMPERATURE AND WIND DIRECTION >iÊ7>ÌiÀÊiÛiÃÊ>`Ê-ÌÀi>ÊÜà (ISTORICALLY WATER LEVELS IN THE 'REAT ,AKES HAVE BEEN HIGHLY VARIABLE AND THERE HAS BEEN NO CLEAR TREND TOWARD LOWER WATER LEVELS FROM TO THE PRESENT %VEN THOUGH WATER LEVELS IN THE 'REAT ,AKES WERE VERY LOW IN FOR INSTANCE LEVELS IN SEVERAL INLAND LAKES IN 7ISCONSIN ROSE DRAMATICALLY FROM TO LARGELY BECAUSE OF INCREASING SNOWFALL RISING GROUND WATER LEVELS AND PRESUMED INCREASES IN GROUNDWATER CONTRIBUTIONS )NDEED UNTIL THE LATE S THE 'REAT ,AKES THEMSELVES HAD EXPERIENCED THREE DECADES OF EXTREMELY HIGH WATER LEVELS 7ATER LEVELS USUALLY RISE IN THE SPRING AS SNOWMELT ENTERS THE LAKES AND DROP IN LATE SUMMER AND FALL AS SURFACE WATER EVAPORATES AND THE WEATHER TURNS DRIER $ESPITE A LACK OF OVERALL TRENDS IN WATER LEVEL THERE HAVE BEEN TRENDS IN THE SEASONAL TIMING OF CHANGING WATER LEVELS FROM THE S TO )N BOTH ,AKES /NTARIO AND %RIE OVER THIS PERIOD THE SEASONAL RISES AND FALLS OF WATER LEVEL ARE OCCURRING ONE MONTH EARLIER THAN BEFORE WHILE IN ,AKE 3UPERIOR THE MAXIMUM WATER LEVEL IS OCCURRING SLIGHTLY EARLIER IN THE YEAR 4HESE TRENDS APPARENTLY RESULT FROM EARLIER SNOWMELT AND EARLIER TAPERING OFF OF SUMMER RUNOFF 4HE FREQUENCY OF HEAVY SUMMER RAINSTORMS HAS INCREASED OVER THE PAST YEARS IN THE 'REAT ,AKES REGION &IGURE P AND mOODING FROM THESE DOWNPOURS WHICH SATURATE SOILS AND CAUSE RAPID RUNOFF MAY BE INCREASING 4HE TREND TOWARD MORE FREQUENT HEAVY RAINSTORMS APPEARS TO HAVE INCREASED mOODING IN SMALL AND MEDIUMSIZED STREAMS IN THE CENTRAL 5NITED 3TATES FROM TO %VEN IF THE CLIMATE TURNS DRIER IN THE FUTURE INCREASED mOODING OF STREAMS AND EROSION OF LAKE SHORES IS LIKELY IF A GREATER PROPORTION OF THE RAIN FALLS IN EXTREME STORM EVENTS &LOODING IS ALSO EXACERBATED BY CONSTRUCTION OF ROADS BUILDINGS AND OTHER IMPERVIOUS SURFACES THAT PREVENT WATER FROM INlLTRATING THE SOIL *ÀiVÌÃÊvÊÕÌÕÀiÊ >ÌiÊÊÌ iÊÀi>ÌÊ>iÃÊ,i} & OR MOST PEOPLE THE CRITICAL IMPACTS OF CLIMATE CHANGE WILL BE THOSE THAT OCCUR AT LOCAL AND REGIONAL SCALES 3OPHISTICATED GENERAL CIRCULA TION MODELS '#-S OF THE %ARTHS CLIMATE SYSTEM ARE THE BEST TOOLS FOR GLOBAL CLIMATE PROJECTIONS 7HILE MOST OF THESE MODELS AGREE ON FUTURE CLIMATE CHANGES FOR THE %ARTH AS A WHOLE REGIONAL PREDICTIONS ARE DIF lCULT BECAUSE THE EXTRAPOLATION FROM LARGE TO LOCAL SCALES IS NOT PRECISE !LSO THE MODELSIMULATED VARI ABILITY AND UNCERTAINTY IN CLIMATE INCREASE AS THE AREA UNDER CONSIDERATION GROWS SMALLER &OR THIS REASON THE CLIMATE CHANGE PROJECTIONS PRESENTED IN THIS REPORT RELY ON MULTIPLE APPROACHES !NALYSES OF REGIONAL TEMPERATURE AND PRECIPITATION PROJECTIONS FROM SEVERAL OF THE MOST UPTODATE '#-S HAVE BEEN COMBINED WITH YEARS OF HISTORICAL DATA FROM THE -IDWEST #LIMATE #ENTER TO SERVE AS A GUIDE TO POSSIBLE FUTURE CHANGES 4HIS REPORT USES RESULTS FROM TWO OF THE LATEST GENERATION OF '#-S THE 0ARALLEL #LIMATE -ODEL 0#- DEVELOPED FOR THE 53 $EPARTMENT OF %NERGY AT THE 53 .ATIONAL #ENTER FOR !TMOSPHERIC 2ESEARCH AND THE (AD#- MODEL DEVELOPED AT THE 5+ -ETEOROLOGICAL /FlCES (ADLEY #ENTRE FOR #LIMATE -ODELING -ODEL SIMULATIONS OF HUMANINDUCED CLIMATE CHANGE MUST RELY ON SOME PLAUSIBLE SCENARIOS ABOUT HOW MUCH #/ THE WORLD WILL BE EMITTING IN THE FUTURE 4HESE EMISSION SCENARIOS ARE IN TURN &OR ADDITIONAL TECHNICAL BACKGROUND ON THE MODELS AND SCENARIOS USED IN THIS REPORT AS WELL AS ADDITIONAL MODELING RESULTS SEE WWWUCSUSAORGGREATLAKES # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA BASED ON ASSUMPTIONS ABOUT SUCH FACTORS AS WORLD POPULATION GROWTH ECONOMIC DEVELOPMENT TECHNOLOGICAL CHANGE AND CONTINUED RELIANCE ON FOSSIL FUELS 4HE CLIMATE ANALYSES IN THIS REPORT ARE BASED ON MODEL RUNS USING SCENARIOS THAT SPAN THE RANGE OF BUSINESSASUSUAL PROJECTIONS MADE BY AN )0## SPECIAL REPORT ON EMISSION SCENARIOS 4HE HIGHEMISSION SCENARIO PROJECTS RAPID ECONOMIC GROWTH AND CONTINUED DEPENDENCE ON FOSSIL FUELS WHILE THE LOWEMISSION SCENARIO FORESEES A MOVE TOWARD CLEAN EFlCIENT TECHNOLOGIES AND SUSTAIN ABLE ECONOMIES #LIMATE MODELS OFTEN DIFFER CONSIDERABLY IN THEIR SENSITIVITY THAT IS IN THE DEGREE OF WARMING THEY PROJECT IN RESPONSE TO INCREASES IN ATMOSPHERIC GREEN HOUSE GASES 7HEN COMPARED WITH THE FULL RANGE OF CLIMATE MODELS THE (AD#-S SENSITIVITY LIES IN THE MIDDLE OF THE RANGE WHILE THE 0#-S SENSITIVITY IS LOW INDICATING THAT THE CLIMATE PROJECTIONS PRESENTED IN THIS REPORT CAPTURE MUCH OF THE RANGE OF PLAUSIBLE CLIMATE FUTURES FOR THIS REGION OVER THE 'REAT ,AKES 1 , Ê £ ä *ÀiVÌi`Ê >}iÃÊÊ/i«iÀ>ÌÕÀiÊ WILL BE TO & TO ÕÀ}Ê-ÕiÀÊ>`Ê7ÌiÀÊLÞÊ # LOWER THAN TEM ÓäÇäqÓäÊ­,i>ÌÛiÊÌʣȣq£ä]Ê PERATURE INCREASES OVER ÛiÀ>}iÊvÀÊÜÊ>`Ê} ÃÃÊ -Vi>Àî THE SOUTHWESTERN AND NORTHERN AREAS OF THE REGION -ICHIGAN NORTH ERN -INNESOTA 7IS CONSIN AND /NTARIO &IGURE )N WINTER THE GREATEST WARMING IS EXPECTED TO OCCUR AT HIGHER LATITUDES 4HIS WILL BE REVERSED FOR SUMMER WITH THE GREAT EST CHANGES OCCURRING -iiÊ«>}iÊÎn OVER THE SOUTHERN AND vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi WESTERN PARTS OF THE REGION )LLINOIS )NDIANA 1 , Ê £ £ ÀÜ}Ê-i>ÃÊÊÌ iÊÀi>ÌÊ -INNESOTA AND /HIO >iÃÊ,i}Ê­£ääqÓ£ää® 4HE SEASONAL CYCLE OF TEMPERATURE OVER THE /i«iÀ>ÌÕÀi REGION IS ALSO PROJECTED 4EMPERATURE IS EXPECTED TO INCREASE THROUGHOUT TO SHIFT WITH SUMMER THE NEXT CENTURY AND TO VARY SUBSTANTIALLY BY SEASON AND TO A LESSER EXTENT "Y BOTH MODELS PROJECT THAT SPRING AND WINTER WARMING MORE SUMMER TEMPERATURES IN THE 'REAT ,AKES REGION ARE THAN SPRING AND FALL LIKELY TO BE TO & TO # ABOVE CURRENT AVER 4HESE PROJECTED AGES 0ROJECTIONS OF FALL AND WINTER TEMPERATURE CHANGE CHANGES IN TEMPERATURE OVER THE NEXT FEW DECADES ARE AMBIGUOUS WITH WARM PATTERNS ARE CONSISTENT ING NOT EVIDENT UNTIL THE MIDDLE OF THE CENTURY "Y WITH RECENT TRENDS IN THE END OF THE CENTURY HOWEVER SUBSTANTIAL TEMPERA GROWING SEASON LENGTH TURE INCREASES ARE EXPECTED IN ALL SEASONS &IGURE AND DATES OF lRST AND LAST -iiÊ«>}iÊÎ vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi 4HE (AD#- MODEL PROJECTS THAT WINTER TEMPERA FROST (ISTORICAL DATA SHOW TURE INCREASES AVERAGED OVER THE PERIOD THAT THE LONGEST GROWING SEASONS OCCURRED IN THE S WILL RANGE FROM TO & TO # IF THE LOWEMIS &IGURE #OMPARED WITH THE TURN OF THE CENTURY SION SCENARIO PREVAILS AND TO & TO # FOR THE GROWING SEASONS TODAY ARE ABOUT ONE WEEK LONGER THE HIGHEMISSION SCENARIO 3UMMER TEMPERATURES PRIMARILY BECAUSE THE LAST SPRING FROST HAS BEEN OC ARE PROJECTED TO INCREASE EVEN CURRING EARLIER -ODEL PRO MORE FOR THE HIGHEMISSION JECTIONS SUGGEST THAT THE ÊiÃÃÊÌ iÊÌ ÀiiÊ`iV>`iÃ]Ê SCENARIO TO & TO LENGTH OF THE GROWING # BUT SLIGHTLY LESS FOR THE ëÀ}Ê>`ÊÃÕiÀÊÌi«iÀ>ÌÕÀiÃÊ SEASON WILL CONTINUE TO LOW SCENARIO TO & TO INCREASE AND BY THE END ÊÌ iÊÀi>ÌÊ>iÃÊÀi}Ê>ÀiÊiÞÊ OF THE CENTURY IT MAY BE # 7ARMING IS EXPECTED TO ÌÊLiÊÎÊÌÊ{cÊ­£°xÊÌÊÓc ®Ê>LÛiÊ TO WEEKS LONGER THAN VARY ACROSS THE REGION 4EM THE AVERAGE VÕÀÀiÌÊ>ÛiÀ>}ið PERATURE INCREASES CENTERED &IGURE 4HE DATE OF # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 3CENARIOS OF #HANGE 1,Ê£Ó *ÀiVÌi`Ê >}iÃÊÊ*ÀiV«Ì>ÌÊ ÕÀ}Ê-ÕiÀÊ>`Ê7ÌiÀÊLÞÊ ÓäÇäqÓäÊ­,i>ÌÛiÊÌʣȣq£ä]Ê ÛiÀ>}iÊvÀÊÜÊ>`Ê} ÃÃÊ -Vi>Àî LAST SPRING FROST IS PROJECTED TO BE EARLIER BY AS MUCH AS TO DAYS AND THE DATE OF lRST AUTUMN FROST IS PROJECTED TO BE LATER BY UP TO DAYS *ÀiV«Ì>Ì]Ê ÝÌÀiiÊÛiÌÃ]Ê >`Ê,Õvv "OTH THE LOW AND HIGHEMISSION SCENARIOS PROJECT THAT AVERAGE ANNUAL PRECIPITATION MAY BE SLIGHTLY ABOVE -iiÊ«>}iÊ{ä AVERAGE RISING TO vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi PERCENT BY THE END OF 1,ʣΠTHE CENTURY &IGURE B -i>Ã>Ê*ÀiV«Ì>ÌÊ ÞViÊ P #HANGES IN THE ­ÃÌÀV>Ê>ÃiiÊ>`Ê*ÀiVÌi`Ê SEASONAL PRECIPITATION >}iÃ]Ê£ä>ÞÊ,Õ}Êi>®Ê CYCLE ARE LIKELY TO BE HIGHER WITH WINTER AND SPRING RAIN INCREASING AND SUMMER RAIN DE CREASING BY UP TO PERCENT 4HE LARGEST PRECIPITATION INCREASES DURING WINTER MONTHS ARE EXPECTED AT HIGHER -iiÊ«>}iÊ{£ LATITUDES AND UNDER THE vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi HIGHEREMISSION SCENARIO &IGURE !LTHOUGH THIS MAY RESULT IN MORE SNOW FALL WARMING TEMPERATURES ARE EXPECTED TO CAUSE A DECREASE IN THE AVERAGE DEPTH OF SNOW COVER DURING THE WINTER )N SUMMER THE LARGEST DECREASES ARE EX PECTED OVER THE SOUTHERN AND WESTERN PARTS OF THE REGION WHERE MOST AGRICULTURE IS CONCENTRATED 0RE CIPITATION IS ALSO PROJECTED TO INCREASE DOWNWIND OF THE 'REAT ,AKES PROBABLY BECAUSE OF THE INmUENCE OF THE LAKES ON LOCAL CONDITIONS UNDER WARMER TEMPERA TURES 4OWARD THE END OF THE CENTURY SPRING AND FALL MAY BE WETTER AND WINTER AND SUMMER DRIER ON AVERAGE ACROSS THE REGION RELATIVE TO TODAYS SEASONAL PATTERNS &IGURE 4HE FREQUENCY OF HEAVY RAINSTORMS BOTH HOUR AND MULTIDAY WILL ALMOST CERTAINLY CONTINUE TO INCREASE DURING THE NEXT CENTURY AND MAY DOUBLE BY &IGURES AND 4HE INTENSITY OF THESE EVENTS MAY INCREASE THOUGH THIS IS ACCORDED A LOWER CON lDENCE LEVEL AND WOULD BE LIKELY TO INCREASE THE RISK OF mOODING 0ERHAPS MOST IMPORTANT TO THE WELFARE OF THE REGION WILL BE THE IMPACTS OF CLIMATE CHANGE ON WATER DISTRIBUTION AND RESOURCES !S CLIMATE WARMS EVAPO TRANSPIRATION IS EXPECTED TO INCREASE YEARROUND WITH THE LARGEST RELATIVE INCREASES IN WINTER AND SPRING %VAPOTRANSPIRATION IS SHORTHAND FOR THE PROCESSES OF EVAPORATION FROM SOILS AND SURFACE WATERS AND TRANS PIRATION OF MOISTURE FROM PLANTS BOTH OF WHICH RE TURN WATER TO THE ATMOSPHERE 4HE DIFFERENCE BETWEEN PRECIPITATION AND EVAPOTRANSPIRATION GIVES AN INDI / iÊvÀiµÕiVÞÊvÊ i>ÛÞÊÀ>ÃÌÀÃ]Ê LÌ ÊÓ{ ÕÀÊ>`ÊÕÌ`>Þ]ÊÜÊ ÊÊÊÊÊÊÊ >ÃÌÊViÀÌ>ÞÊVÌÕiÊÌÊVÀi>ÃiÊ `ÕÀ}ÊÌ iÊiÝÌÊViÌÕÀÞÊ>`Ê>ÞÊ `ÕLiÊLÞÊÓ£ää° CATION OF HOW MUCH WATER IS AVAILABLE FOR RUNOFF INTO STREAMS AND LAKES OR FOR RECHARGING GROUNDWATER SUP PLIES /N AVERAGE OVER THE ENTIRE REGION BY THE END OF THE CENTURY THE AMOUNT OF WATER AVAILABLE FOR RUNOFF IS EXPECTED TO REMAIN THE SAME OR PERHAPS INCREASE FOR ALL SEASONS EXCEPT SUMMER )N SUMMER LESS RUNOFF IS PREDICTED AND CHANGES ARE EXPECTED TO BE HIGHLY VARIABLE ACROSS THE REGION ,ARGE AREAS WHERE RUNOFF IS REDUCED MAY OCCUR ACROSS THE -IDWEST DURING WIN TER AND SUMMER AND IN THE CENTRAL 'REAT ,AKES REGION DURING AUTUMN )N CONTRAST RUNOFF IS PROJECTED TO INCREASE OVER THE ENTIRE REGION DURING SPRING AND OVER THE SOUTHERN 'REAT ,AKES REGION DURING FALL #HANGES IN THE AMOUNT OF WATER AVAILABLE FOR RUNOFF WILL ALSO AFFECT SOIL MOISTURE WHICH IS A KEY FACTOR IN PLANT GROWTH AND SOIL PROCESSES 4HUS SOIL MOISTURE IS PROJECTED TO INCREASE AS MUCH AS PER CENT DURING WINTER IN SOME LOCALES BUT DECREASE RE GIONALLY BY UP TO PERCENT IN SUMMER AND FALL RELA TIVE TO THE n AVERAGE 4HIS SHIFT WILL FAVOR CROPS AND ECOSYSTEMS THAT RELY ON RECHARGE OF WATER LEVELS DURING THE WINTER MONTHS HOWEVER CROPS # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA REQUIRING A CERTAIN LEVEL OF SUMMER RAINFALL AND SOIL MOISTURE MAY COME UNDER SUBSTANTIAL STRESS AND SOME WETLAND ECOSYSTEMS MAY DRY UP ENTIRELY DURING SUMMERS s "Y SOUTHERN /NTARIO SUMMERS MAY FEEL MORE LIKE THOSE IN UPSTATE .EW 9ORK AND BY THE END OF THE CENTURY SIMILAR TO THOSE IN NORTHERN 6IRGINIA TODAY }À>Ì}Ê >Ìià ! DRAMATIC WAY OF VISUALIZING THE EFFECTS OF THESE CLIMATE PROJECTIONS IS TO ESTIMATE WHERE /NTARIO AND SELECTED 'REAT ,AKES STATES WILL HAVE hMOVEDv CLIMATI CALLY OVER THE NEXT CENTURY 3UCH ANALYSES ARE LIMITED OF COURSE TO AVERAGE CONDITIONS AND DO NOT CONSIDER THE EXTREMES OR VARIABILITY IN PROJECTED CLIMATE CHANGES 4HEY ALSO DO NOT TAKE INTO ACCOUNT DIFFERENCES IN MAJOR TOPOGRAPHICAL FEATURES FROM STATE TO STATE SUCH AS THE !PPALACHIANS THE /ZARKS OR THE 'REAT ,AKES 4HAT SAID HERE ARE A FEW COMPARISONS BASED ON PROJECTIONS OF SEASONAL AVERAGE TEMPERATURE AND PRECIPITATION &IGURE / iÊ*ÌiÌ>ÊvÀÊ-ÕÀ«ÀÃi )N ADDITION TO THE GRADUAL LONGTERM TRENDS IN CLIMATE JUST DISCUSSED IT 1,Ê£{ IS POSSIBLE THAT VERY VÀi>Ãi`ÊÀiµÕiVÞÊvÊi>ÛÞÊ,> ABRUPT AND STRONG SHORT v>ÊÛiÌÃÊÊÌ iÊÀi>ÌÊ>iÃÊ,i} TERM CHANGES IN CLIMATE COULD OCCUR AS WELL !N ABRUPT CHANGE IS ONE THAT TAKES PLACE SO RAPIDLY AND UNEXPECTEDLY WITHIN YEARS TO DECADES THAT HUMAN OR NATURAL SYS TEMS HAVE DIFlCULTY ADAPT ING !BRUPT CHANGES IN PAST CLIMATE ARE WELL -iiÊ«>}iÊ{£ vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi DOCUMENTED BY RECORDS PRESERVED IN FOSSILS ICE 1 , Ê £ x CORES AND LAKE SEDIMENTS *ÀiV«Ì>ÌÊ- vÌÃÊ-}>Ê/ÀÕLiÊ 0ATTERNS OF ABRUPT CHANGE vÀÊ>ÀiÀà FROM GLACIAL TO INTER GLACIAL PERIODS WERE COM MON FOR EXAMPLE WITH SUDDEN CHANGES IN THE .ORTH !TLANTIC RAPIDLY AFFECTING THE ENTIRE .ORTHERN (EMISPHERE INCLUDING THE 'REAT ,AKES REGION 4EMPER ATURES SHOT UP BY AS -iiÊ«>}iÊ{Ó vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi MUCH AS & # AND RAINFALL DOUBLED IN 1,Ê£È A MATTER OF DECADES IN }À>Ì}Ê >Ìi\Ê >}}Ê SOME REGIONS IN RE 7ÌiÀÃÊ>`Ê-ÕiÀÃÊÊÃÊ SPONSE TO THE WARMING >`ÊV }>Ê OF .ORTH !TLANTIC SUR FACE WATERS AFTER THE ICE SHEETS MELTED )N THE PAST ABRUPT CHANGES OCCURRED MOST OFTEN WHEN THE CLIMATE SYSTEM WAS BEING FORCED -iiÊ«>}iÊ{Ó TO CHANGE RAPIDLY BY vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi s "Y A TYPICAL WINTER CLIMATE IN THE STATE OF )LLINOIS CAN BE EXPECTED TO FEEL HOTTER AND DRIER MUCH LIKE CURRENTDAY /KLAHOMA OR !RKANSAS s "Y TODAYS -ICHIGAN WINTER CLIMATE IS LIKELY TO BE REPLACED BY A CLIMATE SIMILAR TO THAT IN /HIO TODAY s 3UMMER CHANGES WILL APPEAR MORE QUICKLY "Y )LLINOIS SUMMERS MAY RESEMBLE THOSE OF /KLAHOMA OR !RKANSAS IN TERMS OF AVERAGE TEM PERATURE AND RAINFALL (OWEVER BY THE END OF THE CENTURY THE )LLINOIS SUMMER CLIMATE WILL GENERALLY RESEMBLE THAT OF CURRENT EAST 4EXAS s -ICHIGAN SUMMER WEATHER COULD BE SIMILAR TO THAT OF /HIO IN A FEW DECADES WHILE BY THE END OF THE CENTURY -ICHIGAN SUMMERS ARE LIKELY TO RESEMBLE THOSE OF NORTHERN !RKANSAS TODAY ÞÊViÌÕÀÞ½ÃÊi`]ÊÃÕiÀÃÊÊ ÊÊÊÊÊÊÊÊÊÊÊ ÃÊÜÊ}iiÀ>ÞÊÀiÃiLiÊÌ ÃiÊ vÊi>ÃÌÊ/iÝ>ÃÊÌ`>Þ]ÊÜ iÊV }>Ê ÃÕiÀÃÊ>ÀiÊiÞÊÌÊÀiÃiLiÊ Ì ÃiÊÀ>Ã>ÃÊÜÊiÝ«iÀiVið # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 3CENARIOS OF #HANGE NATURAL FORCES SUCH AS METEOR IMPACTS OR MAJOR VOLCANIC ERUPTIONS .OW IT IS AGAIN FORCED TO CHANGE RAPIDLY BUT BY A COMBINATION OF NATURAL AND HUMAN FORCES ! RECENT REPORT ON ABRUPT CLIMATE CHANGE CONCLUDED hGREENHOUSE WARMING AND OTHER HUMAN ALTERATIONS OF THE EARTH SYSTEM MAY INCREASE THE POSSIBILITY OF LARGE ABRUPT AND UNWELCOME REGION AL OR GLOBAL CLIMATIC EVENTSv !BRUPT CHANGES IN CLIMATE COULD OBVIOUSLY HAVE DRAMATIC IMPACTS ON THE 'REAT ,AKES REGION LEAVING EVEN LESS TIME FOR SOCIETY THE ECONOMY AND NATURAL ECOSYSTEMS TO ADAPT OR MITIGATE THE DAMAGE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA #(!04%2 4HREE %COLOGICAL 6ULNERABILITY TO #LIMATE #HANGE !QUATIC %COSYSTEMS 4 HE 'REAT ,AKES REGION IS DISTINGUISHED BY ITS ABUNDANT LAKES STREAMS AND WETLANDS !LL OF THESE AQUATIC ECOSYSTEMS WILL BE AFFECTED IN SOME WAY BY THE DIRECT HUMAN STRESSES AND HUMANDRIVEN CLIMATE CHANGES EXPLORED IN #HAPTERS AND >iÊVÃÞÃÌià , AKES IN THE REGION DIFFER WIDELY IN SIZE DEPTH TRANSPARENCY AND NUTRIENT AVAILABILITY CHARAC TERISTICS THAT FUNDAMENTALLY DETERMINE HOW EACH LAKE WILL BE AFFECTED BY CLIMATE CHANGE &IGURE ! WIDE VARIETY OF STUDIES HAVE FOCUSED ON THE INLAND WATERS AND 'REAT ,AKES PROVIDING STRONG EVI DENCE OF HOW THE WATERS HAVE CHANGED AND ARE LIKELY TO CHANGE IN THE FUTURE } iÀÊ>iÊ/i«iÀ>ÌÕÀià 7ARMER AIR TEMPERATURES ARE LIKELY TO LEAD TO INCREAS ING WATER TEMPERATURES AND CHANGES IN SUMMER STRAT IlCATION IN THE 'REAT ,AKES AND IN THE INLAND LAKES AND STREAMS OF THE REGION %ARLIER MODEL STUDIES PROJECT THAT SUMMER SURFACE WATER TEMPERATURES IN INLAND LAKES WILL INCREASE BY TO & TO # 0ROJECTIONS FOR DEEP WATER RANGE FROM A & WARM ING TO A COUNTERINTUITIVE & COOLING 4HE RESPONSE IN DEEP WATERS VARIES BECAUSE WARMING AIR TEMPERA TURES CAN CAUSE A SMALL DEEP LAKE TO STRATIFY SOONER IN SPRING AT A COOLER TEMPERATURE 0ROJECTED CHANGES IN WATER TEMPERATURE WOULD BE EVEN GREATER USING THE MORE RECENT CLIMATE SCENARIOS ON WHICH THIS REPORT IS BASED ESPECIALLY BY /VERALL CHANGES IN TEM PERATURE AND STRATIlCATION WILL AFFECT THE FUNDAMENTAL PHYSICAL CHEMICAL AND BIOLOGICAL PROCESSES IN LAKES SEE BOX P (IGHER WATER TEMPERATURES FOR EXAMPLE RESULT IN LOWER OXYGEN LEVELS ,OWER OXYGEN AND WARMER TEMPERATURES ALSO PROMOTE GREATER MICRO 1 , Ê £ Ç BIAL DECOMPOSITION AND «>VÌÃÊÊ>iÊVÃÞÃÌià SUBSEQUENT RELEASE OF NUTRIENTS AND CONTAMI NANTS FROM BOTTOM SEDI MENTS 0HOSPHORUS RE LEASE WOULD BE ENHANCED AND MERCURY RELEASE AND UPTAKE BY BIOTA WOULD ALSO BE LIKELY TO INCREASE /THER CONTAMINANTS PARTICULARLY SOME HEAVY METALS WOULD BE LIKELY TO RESPOND IN A SIMILAR FASHION (EAVY METALS SUCH AS MERCURY BECOME MORE SOLUBLE IN THE ABSENCE OF OXYGEN /XY GEN BINDS WITH THESE ELEMENTS TO FORM IN SOLUBLE COMPOUNDS THAT -iiÊ«>}iÊ{Ó SINK TO THE BOTTOM vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA !QUATIC %COSYSTEMS PERSIST IN LAKES THAT PREVIOUSLY EXPERIENCED WINTERKILL 2EDUCED ICE COVER ALSO ALLOWS GREATER STORM DISTUR BANCE WHICH INCREASES EGG MORTALITY OF THE COMMER CIALLY VALUABLE LAKE WHITElSH WHOSE EGGS INCUBATE OVER WINTER ON THE BOTTOM OF 'REAT ,AKES BAYS )NCREASES IN THE ICEFREE PERIOD EXTEND THE SHIPPING SEASON ON THE 'REAT ,AKES BUT REDUCE ICE lSHING ICE BOATING SKIING SNOWMOBILING AND WINTER FESTIVALS SUCH AS 7ISCONSINS h+ITES ON )CEv SEE BOX P USED IN THIS REPORT (AD#- SUGGEST EVEN GREATER DECLINES IN LATE SUMMER WATER LEVELS BECAUSE THIS MODEL PROJECTS HIGHER TEMPERATURES AND LOWER SUMMER RAIN FALL IN THE REGION THAN THE MODELS USED IN PREVIOUS STUDIES (OWEVER THE ABSENCE OF LONGTERM TRENDS IN THE HISTORIC 'REAT ,AKES WATER LEVELS RECORD AND INCREASES IN WATER IN SOME INLAND AREAS OF 7ISCONSIN SUGGEST THAT LAKE WATER LEVELS MAY NOT YET SHOW THE DECLINE EXPECTED FROM LONGTERM CLIMATE CHANGE >}iÃÊÊ>iÊ7>ÌiÀÊiÛiÃÊ #LIMATE SCENARIOS AND LAKE MODELS HAVE CONSISTENTLY PREDICTED LESS RUNOFF MORE EVAPORATION AND LOWER WATER LEVELS IN BOTH LARGE AND SMALL LAKES IN THE REGION 4HE MOST RECENT HYDROLOGIC MODELS CONTINUE TO PRO JECT LOWER LAKE AND GROUNDWATER LEVELS IN THE FUTURE 4ABLE DESPITE A LACK OF CLEAR TRENDS IN THE HISTORIC RECORD 0REDICTIONS BASED ON ONE OF THE CLIMATE MODELS >}iÃÊÊ>iÊ*À`ÕVÌÛÌÞ 4HE GROWTH OF ALGAE IN THE WATER AND ON LAKE BOTTOMS IS CALLED PRIMARY PRODUCTION BECAUSE THESE PLANKTONIC PLANTS FORM THE BASE OF THE FOOD WEB THAT NOURISHES ANIMALS FROM ZOOPLANKTON TO lSH 0RIMARY PRODUC TION IS CONTROLLED BY A COMBINATION OF TEMPERATURE LIGHT OR THE PORTION OF THE ICEFREE YEAR WHEN LIGHT IS AVAILABLE AND NUTRIENTS %XCESSIVE NUTRIENTS CAN /Ê£ÊÊÊViÊ ÛiÀÊÝ«iVÌi`ÊÌÊiVÀi>ÃiÊÊÌ iÊÀi>ÌÊ>iÃÊ,i} >i ÕÀÀiÌÊ-ÌÕ>Ì >iÃÊ-Õ«iÀÀÊ >`ÊÀiÊ­ÈÊL>Ãî> ÇÇÊÌÊ£££Ê`>ÞÃÊ vÊViÊVÛiÀ iVÀi>ÃiÊViÊVÛiÀÊ vÀÊ££xnÊ`>ÞÃÊ iVÀi>ÃiÊViÊVÛiÀÊ vÀÊÎÎnnÊ`>ÞÃÊ >iÊ-Õ«iÀÀÊ ­ÎÊL>Ãî> ÊVivÀiiÊ ÜÌiÀà VÀi>ÃiÊVivÀiiÊÜÌiÀÃÊ vÀÊä{¯ VÀi>ÃiÊVivÀiiÊÜÌiÀÃÊ vÀÊ{{x¯ >iÊÀiÊ ­ÎÊL>Ãî> Ó¯ÊvÊÜÌiÀÃÊ >ÀiÊViÊvÀii äÈ£¯ÊvÊÜÌiÀÃÊ >ÀiÊVivÀiiÊ {ȯÊvÊÜÌiÀÃÊ >ÀiÊVivÀiiÊ ->Ê>`Ê>iÃL Hä£ääÊ`>ÞÃÊ vÊViÊVÛiÀ iVÀi>ÃiÊViÊVÛiÀÊLÞÊ{xÈäÊ`>ÞÃÊÜÌ Ê>Ê`ÕL}Ê vÊ>Ìë iÀVÊ "Ó ÞÊÓäÎä ÕÌÕÀiÊ-Vi>Àà ÞÊÓää -ÕÀVi\Ê-iiÊÌiÊÈ£° /ÊÓÊÊÊ7>ÌiÀÊiÛiÃÊiÞÊÌÊiVÀi>ÃiÊÊÌ iÊÕÌÕÀiÊ­>ÃÊà ÜÊ iÀiÊvÀÊÌ iÊÀi>ÌÊÊ Ê>iÃ]Ê ÀÞÃÌ>Ê>i]Ê7ÃVÃ]Ê>`Ê}ÀÕ`Ü>ÌiÀÊi>ÀÊ>ÃÌÊ>Ã}]ÊV }>®Ê >iÊÀÊ-Ìi ÓÊÊ "Ó ­À>}iÊvÊÎ{ÊÃÕ>Ìî ÓäÎäÊ ­À>}iÊvÊÓÊÃÕ>Ìî ÓääÊ ­À>}iÊvÊÓÊÃÕ>Ìî >iÊ-Õ«iÀÀ qä°ÓÎÊÊÌÊqä°{ÇÊ qä°ä£ÊÊÌÊqä°ÓÓÊ ³ä°££ÊÊÌÊqÊä°{ÓÊ >iÊÕÀÉV }> qä°ÊÊÌÊqÓ°{nÊ ³ä°äxÊÊÌÊqä°ÇÓÊ ³ä°ÎxÊÊÌÊqÊ£°ÎnÊ ÀÞÃÌ>Ê>i]Ê 7ÃVà q£°äÊÊÌÊq£°Ê ­ÓÊÃÕ>Ìî ÀÕ`Ü>ÌiÀÊi>ÀÊ >Ã}]ÊV }> qä°ÈÊÌÊ³ä°£Ê -ÕÀVi\Ê-iiÊÌiÊÈÓ°Ê``Ì>Ê`>Ì>ÊÊ>iÊiÛiÊ`iViÃÊV>ÊLiÊvÕ`ÊÊÌ iÊÌiV V>Ê>««i`ViÃ\Ê ÌÌ«\ÉÉÜÜÜ°ÕVÃÕÃ>°À}É}Ài>Ì>iÃÉ}V >i}iÌiV L>V° Ì # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA MODEL PREDICTIONS FOR THE REGION ALSO SUGGEST THAT OVER THE NEXT YEARS PRECIPITATION WILL INCREASE DURING WINTER AND SPRING 4HIS COULD INCREASE THE MAGNITUDE OF SPRING mOODS ESPECIALLY IF THE mOODS COINCIDE WITH SNOWMELT WHEN SOILS ARE STILL FROZEN 3TREAM RESPONSES TO THESE CLIMATEDRIVEN CHANGES WILL VARY GREATLY ACROSS THE REGION 4ABLE MAINLY BECAUSE OF DIFFERENCES IN THE RELATIVE CONTRIBUTION OF GROUNDWATER VERSUS SURFACE WATER TO THEIR mOW PATTERNS $IRECT HUMAN DISTUR BANCES SUCH AS REMOVING STREAMSIDE VEGETATION PAVING OR DEVELOPING LAND CHANNELIZING STREAMS DEPOSITING NITROGEN AND ACID FROM ACID RAIN DIVERTING WATER AND INTRODUCING INVASIVE SPECIES WILL UNDOUBTEDLY ALTER THE WAY STREAM ECOSYSTEMS RESPOND TO CLIMATE CHANGE «>VÌÃÊvÊ >}iÃÊÊÞ`À}ÞÊ (EAVY RAINFALL EVENTS AND mOODING ARE INCREASING IN THE 'REAT ,AKES REGION SEE &IGURE P AND PROJECTED INCREASES IN THE FREQUENCY OF THESE EVENTS MAY AMPLIFY THE RANGE OF CONDITIONS THAT MAKE mOOD ING MORE LIKELY IN THE FUTURE SUCH AS STREAM CHANNEL ING AND LANDUSE CHANGES THAT INCREASE THE AMOUNT OF IMPERVIOUS SURFACES 4HE LIKELIHOOD OF mOODING WILL ALSO INCREASE WITH CHANGES IN LAND USE 3TREAMS IN THE AGRICULTURAL AREAS ON lNETEXTURED SOILS AND mAT TOPO GRAPHY AT THE EASTERN END OF ,AKE %RIE FOR INSTANCE RISE QUICKLY IN RESPONSE TO RAIN AND ARE LIKELY TO BE ESPECIALLY VULNERABLE TO INTENSE SUMMER STORMS &LOODS EXERT THEIR GREATEST PHYSICAL INmUENCE BY RESHAPING RIVER CHANNELS INUNDATING mOODPLAINS AND MOVING LARGE WOODY DEBRIS AND SEDIMENTS &LOODING CAN DEGRADE WATER QUALITY WHEN UNTREATED HUMAN COMMERCIAL OR AGRICULTURAL WASTES OVERmOW FROM TREATMENT FACILITIES OR WHEN SOILS ARE ERODED FROM AGRICULTURAL lELDS TREATED WITH PESTICIDES AND FERTI LIZERS (IGH WATER mOW ALSO DIMINISHES THE CAPACITY OF A STREAM TO RECYCLE NUTRIENTS AND SEQUESTER SUS PENDED OR DISSOLVED ORGANIC MATTER #HANNELIZED URBAN AND AGRICULTURAL STREAMS HAVE LITTLE CAPACITY TO RETAIN WATER AND THE ANTICIPATED INCREASES IN SPRING RUNOFF BY THE END OF THE CENTURY WILL RESULT IN INCREASED HEIGHT OF SPRING mOODS AND LOWER NUTRIENT AND SEDIMENT RETENTION IN THESE STREAMS .OT ALL IMPACTS OF mOODING ARE NEGATIVE OF COURSE !QUIFER RECHARGE IS ONE BENElT &LOODS ALSO TRANSPORT lNE SEDIMENTS DOWNSTREAM INCREASING THE QUALITY AND QUANTITY OF HABITAT FOR SOME lSH AND INVERTEBRATES )N ADDITION SEVERAL IMPORTANT lSH SPECIES MOVE UPSTREAM INTO THE 'REAT ,AKES TRIBU TARIES TO REPRODUCE DURING SPRING STURGEON WALLEYE AND WHITE SUCKER OR FALL STEELHEAD #HINOOK SALMON AND BROOK TROUT CUED BY EITHER INCREASED mOW OR DAY LENGTH !LTHOUGH CHANGES IN THE FREQUENCY AND SEVERITY OF DISTURBANCES SUCH AS mOODS CAN DISRUPT SOME AQUATIC COMMUNITIES MANY lSH AND INVERTE BRATE SPECIES COEVOLVED WITH SEASONAL mOOD PULSES TO TAKE ADVANTAGE OF THE 1,Ê£ EXPANDED HABITAT FOR «>VÌÃÊÊ-ÌÀi>ÊVÃÞÃÌià SPAWNING AND NURSERY SITES )N THE 'REAT ,AKES REGION THESE SPECIES IN CLUDE BASS CRAPPIE SUN lSH AND CATlSH !PART FROM EXTREME EVENTS SUMMER RAINFALL IS EXPECTED TO DECLINE IN THE FUTURE ESPECIALLY IN THE SOUTHERN AND WESTERN PORTIONS OF THE REGION SEE &IGURE P -iiÊ«>}iÊ{{ $RIER CONDITIONS WILL TRANS vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi LATE INTO LOWER SUMMER STREAM mOW AND LESS STREAM HABITAT (EADWATER STREAMS WHICH OFTEN MAKE UP MORE THAN PERCENT OF THE RIVER MILES IN A WATERSHED ARE PROBABLY THE MOST VULNERABLE OF ALL AQUATIC ECOSYSTEMS UNDER WARMER AND DRIER CONDITIONS &IGURE $ROUGHT EFFECTS CAN LEAD TO WARMER WATER TEMPERATURES DE PLETED OXYGEN HIGHER CONCENTRATIONS OF CONTAMINANTS AS WATER VOLUME DECLINES REDUCED TRANSPORT OF NU TRIENTS AND ORGANIC MATTER AND DISRUPTION OF FOOD WEBS 2EGIONS WITH INTENSIVE AGRICULTURAL PRODUC TION ON lNE SOILS AND mAT TOPOGRAPHY SUCH AS THOSE FOUND AT THE EASTERN END OF ,AKE %RIE WILL BE MOST VULNERABLE TO EXTREME EVENTS AND REDUCED SUMMER RAINFALL SINCE THEIR HYDROLOGY IS CONTROLLED LARGELY BY SURFACE WATER )N SMALL STREAMS WHERE mOW COMES PRIMARILY FROM SURFACE RUNOFF ONE STUDY PREDICTS THAT PERCENT OF THE STREAMS WILL STOP mOWING IF ANNUAL RUNOFF DECREASES BY PERCENT /NE CONSEQUENCE OF PERIODIC DROUGHTS IS THAT SULFATES AND ACIDITY ARE MOBILIZED DURING POSTDROUGHT RAINS AND CAN DELIVER A STRONG ACID PULSE TO STREAMS AND LAKES IN THE WATERSHED "ECAUSE OF THIS PHENOM # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA !QUATIC %COSYSTEMS ENON CLIMATE WARMING MAY SLOW OR EVEN HALT THE RECOVERY OF MANY ACIDSTRESSED AQUATIC ECOSYSTEMS 3TREAMS MOST SUSCEPTIBLE TO ACID RAIN INCLUDE THOSE ON THE #ANADIAN SHIELD OF /NTARIO ALONG THE HIGHER GRADIENT REACHES OF .EW 9ORK AND IN NORTHERN -ICHIGAN -INNESOTA AND 7ISCONSIN «>VÌÃÊvÊ} iÀÊ7>ÌiÀÊ/i«iÀ>ÌÕÀi !CROSS THE WATERSHED STREAM TEMPERATURES WILL CLOSE LY MIRROR INCREASING AIR TEMPERATURES ALTHOUGH THE WARMING MAY BE MODIlED BY SHADE FROM RIPARIAN FORESTS AND OTHER VEGETATION AND BY WATER STORAGE IN WETLANDS ,OCALLY COOL GROUNDWATER SEEPS WILL PROVIDE SOME BUFFERING FOR STREAMS AGAINST WARMING AIR TEMPERATURES 7ARMER WATER WILL AFFECT STREAM ORGANISMS FROM PLANKTON TO INSECTS AND lSH lSH ARE DISCUSSED BELOW )N RESPONSE TO WARMER WATERS SOME INSECT SPECIES INCREASE GROWTH RATES EMERGE EARLIER ARE SMALLER AT MATURITY ALTER THEIR SEX RATIOS OR REDUCE FECUNDITY 0LANKTON PRODUCTIVITY TENDS TO INCREASE WITH WARMER TEMPERATURES AND LONGER GROWING SEASONS BUT REDUCTIONS IN WATER VOLUME COUPLED /ÊxÊÊÊ«>VÌÃÊvÊ >ÌiÊ >}iÊÊ7iÌ>`ÊVÃÞÃÌiÃÊ >Ìi ÀÛiÊ >}i iÞÊ«>VÌÃÊÊ * ÞÃV>Ê*À«iÀÌià iÞÊ«>VÌÃÊÊVÃÞÃÌià >ÀiÀÊViÕÌÊ >`ÊÃÜÊiÌ 7iÌÊ«iÀ`ÃÊ>ÀiÊà ÀÌiÀ]Ê iëiV>ÞÊÊi« iiÀ>Ê ÜiÌ>`Ã°Ê >ÃÌ`iÛi«}ÊÃiVÌÊ>`Ê>« L>Ê Ã«iViÃÊ>ÀiÊv>ÛÀi`]Ê>ÃÊ>ÀiÊëiViÃÊÜÌ Ê ÀiÃÌ}ÊÃÌ>}iÃ°Ê / iÊÌ}ÊvÊ>« L>Ê>`ÊÃiVÌÊviÊ VÞViÃÊVÕ`ÊLiÊ`ÃÀÕ«Ìi`° ÜiÀÊÃÕiÀÊ Ü>ÌiÀÊiÛià Ã>ÌÊ>`Ê vÀ>}iÌ>ÌÊÜÌ Ê ÜiÌ>`ÊV«iÝiÃÊ VÀi>Ãi°Ê iÃÊÃÌÀiÊiÃÃÊV>ÀL°Ê 7>ÀiÀÊ Ìi«iÀ>ÌÕÀià >LÌ>ÌÊ>`Ê}À>ÌÊVÀÀ`ÀÃÊ>ÀiÊ Ài`ÕVi`]Ê>ÃÊ>ÀiÊ Þ`À}VÊViVÌÃÊÌÊ À«>À>ÊâiÃÊ>`Ê}ÀÕ`Ü>ÌiÀÊÀiV >À}i°Ê iÀ}iÌÊÛi}iÌ>ÌÊ>`Êà ÀÕLÃÊ `>ÌiÊ«>ÌÊVÕÌiÃ°Ê ,i`ÕVÌÃÊÊ`ÃÃÛi`Ê À}>VÊV>ÀLÊÀiÃÕÌÊ ÊiÃÃÊ>ÌÌiÕ>ÌÊvÊ ÕÌÀ>ÛiÌÊÀ>`>Ì° « L>Ê>`ÊwÊà ÊÀi«À`ÕVÌÊ v>ÃÊÀiÊvÌiÊÊ`ÀÞÊÞi>ÀÃ°Ê Û>«À>ÌÛiÊÃÃiÃÊ VÀi>Ãi°Ê / iÊÀ>ÌiÃÊvÊ`iV«ÃÌÊ >`ÊÀiëÀ>ÌÊVÀi>Ãi°Ê iÃÊ>`ÊL}ÃÊ ÃÌÀiÊiÃÃÊV>ÀL° ÃiVÌÃÊiiÀ}iÊi>ÀiÀ°Ê ÌiÃvÞ}ÊÀÊ vÕ`}Ê6>À>Lià -ÜiÌÊVVÕÀÃÊ i>ÀiÀÊ>`Êv>ÃÌiÀÊÊ ÕÀL>Ê>Ài>ÃÊ>`ÊÜ iÀiÊ VviÀÕÃÊvÀiÃÌÊ >ÀÛiÃÌÊ >ÃÊVVÕÀÀi`° }ÀVÕÌÕÀ>Ê>`Ê ÕÀL>Ê`iÛi«iÌÊ iÝ>ViÀL>ÌiÊvÀ>} iÌ>ÌÊivviVÌð "À}>ÃÃÊÜÌ Ê«ÀÊ`ëiÀÃ>Ê >LÌiÃÊLiViÊiÝÌVÌ° *À>ÀÞÊ>`ÊÃiV`>ÀÞÊ«À`ÕVÌÊ «iÀÊÕÌÊvÊL>ÃÃÊVÀi>ÃiÊÜ iÊ ÕÌÀiÌÃÊ>ÀiÊÌÊÌi`°Ê «iÀÛÕÃÊÃÕÀv>ViÃÊ VÀi>ÃiÊÜ>ÌiÀÊ Ìi«iÀ>ÌÕÀi°Ê ÀiÊV«iÌÌÊvÀÊ Û>ÃÛiÊëiViÃÊ>ÞÊ >VViiÀ>ÌiÊiÝÌVÌð -«iViÃÊ>ÌÊÌ iÊÃÕÌ iÀÊiÝÌiÌÊ vÊÌ iÊÀ>}iÊLiViÊiÝÌVÌ° ÀiÊvÀiµÕiÌÊ i>ÛÞÊÀ>v>Ê iÛiÌà iÛ>Ìi`Ê >Ìë iÀVÊ "Ó 7iÌ>`ÃÊ VÀi>ÃiÊÊiÝÌiÌ°Ê >LÌ>ÌÊ>Ài>ÊVÀi>ÃiÃ°Ê ÀÕ`iÃÌ}ÊLÀ`ÃÊ>ÞÊ LiÊÃÌÊ`ÕÀ}ÊyÊ`ð 7iÌ>`ÊÃÃiÃÊvÀÊ `iÛi«iÌÊÀi`ÕViÊ yÊ`ÊÃÌÀ>}iÊV>«>VÌÞ° *ÃÃLiÊV >}iÃÊÊi>vÊÌÌiÀʵÕ>ÌÞÊ VÕ`Ê«>VÌÊ>µÕ>ÌVÊv`ÊÜiLð # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA WITH POSSIBLY INTERMITTENT mOW IN SMALLER STREAMS SHOULD LEAD TO REDUCTIONS IN OVERALL AQUATIC PRODUCTION 4HE EFFECTS OF INCREASING WATER TEMPERATURE WOULD BE COMPOUNDED BY FOREST HARVEST ESPECIALLY OF CONI FERS WHICH OPENS UP THE CANOPY AND PROMOTES EAR LIER SNOWMELT .ORTHERN -ICHIGAN -INNESOTA 7IS CONSIN AND WESTERN /NTARIO WILL BE MOST VULNERABLE TO THIS PHENOMENON 5RBAN AREAS ALSO EXPERIENCE EARLIER AND FASTER SNOWMELT THAN DO RURAL AREAS 7ARMER TEMPERATURES SHOULD ENHANCE DECOM POSITION AND NUTRIENT CYCLING IN STREAMS ALLOWING MICROBES TO BREAK DOWN HUMAN AND AGRICULTURAL WASTES INTO NUTRIENTS THAT FUEL GREATER PRIMARY PRODUC TIVITY (OWEVER OTHER IMPACTS OF CLIMATE CHANGE SUCH AS PROLONGED LOW mOWS COMBINED WITH HIGHER TEMP ERATURES MAY LEAD TO OXYGEN DEPLETION WHICH WILL SLOW DECOMPOSITION AND WASTEPROCESSING FUNCTIONS «>VÌÃÊÊ`ÛiÀÃÌÞÊ>`Ê`Ê7iLà ! WARMER CLIMATE WILL COMBINE WITH LANDUSE CHANGE AND THE INTRODUCTION OF INVASIVE SPECIES TO POSE GREAT THREATS TO AQUATIC BIODIVERSITY IN THE COMING CENTURY .ATIVE PLANT AND ANIMAL SPECIES WILL DIFFER WIDELY IN THEIR RESPONSES TO CHANGING STREAM TEMPERATURE AND HYDROLOGY 3OME WILL RESPOND BY ADAPTING TO WARMER TEMPERATURES OR EXPANDING THEIR RANGES NORTHWARD OR SEEKING REFUGE IN AREAS WHERE TEMPERATURES AND mOW PATTERNS REMAIN SUITABLE /THERS WILL DECLINE TO EXTINCTION )NSECTS AND PLANTS THAT HAVE RESISTANT OR MOBILE LIFE HISTORY STAGES LARVAE CYSTS SEEDS WILL SURVIVE BETTER THAN OTHER ORGANISMS DURING REDUCED WATER mOWS &ISH SPECIES PRESUMED TO BE AT HIGHER RISK OF EXTINCTION ARE THOSE THAT HAVE SMALL GEOGRAPHIC RANGES REQUIRE STEADY WATER mOWS OR SLACK WATER HABITATS REPRODUCE AT AN OLDER AGE OR REQUIRE SPECIlC FOODS /F lSH SPECIES IN 7ISCONSIN PERCENT HAVE TWO OR MORE OF THE 1 , Ê Ó ä ABOVE TRAITS INDICATING «>VÌÃÊÊ7iÌ>`ÊVÃÞÃÌià POTENTIAL SENSITIVITY TO GLOBAL WARMING $ARTERS AND SEA LAMPREYS ARE AMONG THE SPECIES THAT ARE ESPECIALLY SENSITIVE !NOTHER POTENTIAL IMPACT ON STREAM FOOD WEBS AND THE BIODIVERSITY THEY SUPPORT COMES DIRECTLY FROM INCREASING ATMOSPHERIC #/ LEVELS 3OME STUDIES INDICATE -iiÊ«>}iÊ{{ vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi THAT PLANT LEAVES GROWN UNDER ELEVATED #/ HAVE LOWER FOOD VALUE )F THESE CHANGES IN LEAF CHEMISTRY TURN OUT TO BE SIGNIlCANT THEY COULD SLOW MICROBIAL DECOMPOSITION OF PLANT MATERIAL THAT FALLS INTO STREAMSA MAJOR SOURCE OF ENERGY AND NUTRIENTS IN MANY AQUATIC ECOSYSTEMS AND ALSO REDUCE GROWTH AND SURVIVAL IN SOME STREAM INSECTS THAT FEED ON THE LEAVES !NY SUCH IMPACTS WOULD BE MAGNIlED UP THE FOOD CHAIN 7iÌ>`ÊVÃÞÃÌià " ECAUSE OF LOW TOPOGRAPHY OR THE PRESENCE OF IMPERVIOUS SOILS THE 'REAT ,AKES REGION HIS TORICALLY HARBORED EXTENSIVE EXPANSES OF WET LANDS PARTICULARLY IN THE PRAIRIE REGIONS OF -INNESOTA AND )LLINOIS THE BOREAL REGIONS OF NORTHERN -INNESOTA AND /NTARIO AND THE LOWLYING FRINGES OF ,AKE -ICHI GAN &IGURE AND ,AKE %RIE INCLUDING THE 'REAT "LACK 3WAMP IN WESTERN /HIO &OR MORE THAN A CEN TURY HOWEVER THESE WETLANDS HAVE BEEN EXTENSIVELY MODIlED OR DRAINED FOR URBAN DEVELOPMENT AND AGRICULTURAL PRODUCTION RESULTING IN TO PERCENT LOSSES IN WETLAND AREA IN THE 'REAT ,AKES STATES AND /NTARIO 4HESE LOSSES ARE ESPECIALLY APPARENT IN THE SOUTHERN PORTION OF THE REGION 7ETLANDS NEAR THE 'REAT ,AKES OCCUR AS THREE DISTINCT TYPES FRINGING COASTAL MARSHES THAT ARE DIRECT LY IMPACTED BY LAKE LEVELS AND WAVE ACTION RIVERINE WETLANDS THAT ARE PARTIALLY INmUENCED BY BOTH LAKE AND RIVER AND PROTECTED LAGOONS OR BARRIER BEACH SYSTEMS THAT ARE HYDROLOGICALLY CONNECTED TO THE LAKE ONLY VIA GROUNDWATER 7HERE THEY HAVE NOT DISAP PEARED COASTAL MARSHES IN THE SOUTHERN PART OF THE BASIN PARTICULARLY ON ,AKE %RIE AND SOUTHERN ,AKE /NTARIO HAVE BEEN EXTENSIVELY DIKED TO PROTECT THEM FROM WATER LEVEL mUCTUATIONS #OASTAL WETLANDS SUCH AS THOSE IN 3AGINAW "AY AND LARGE ESTUARIES SUCH AS 'REEN "AY ARE HOT SPOTS OF PRIMARY PRODUCTIVITY BE CAUSE NUTRIENTS AND SEDIMENTS FROM THROUGHOUT THE # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA EPHEMERAL WETLANDS FOR EXAMPLE WILL THREATEN REPRO DUCTIVE SUCCESS OF CERTAIN SPECIES SUCH AS WOOD FROGS AND MANY SALAMANDERS IN THE 'REAT ,AKES REGION &IGURE )N TIMES OF DROUGHT WHEN INDIVIDUAL WETLANDS ARE ISOLATED FROM ONE ANOTHER DEEP WETLANDS SERVE AS A SAFE HAVEN OR hREFUGIAv FOR PLANTS AND ANIMALS UNTIL WATER LEVELS ARE RESTORED IN DRIEDOUT WETLANDS ,OSS OF THESE REFUGIA DURING LONGER OR MORE SEVERE DROUGHTS WILL THREATEN POPULATIONS OF AMPHIBIANS AND OTHER LESSMOBILE SPECIES ,ANDSCAPE FRAGMENTATION EXACER BATES THIS SITUATION LEAVING REFUGIA SCARCER AND MORE ISOLATED 7ETLAND LOSS AND DEGRADATION ALSO THREATEN TO DRIVE THE YELLOWHEADED BLACKBIRD LOCALLY EXTINCT IN THE 'REAT ,AKES REGION 4HIS SONGBIRDS HABITAT IS RESTRICTED TO A SMALL SUBSET OF MARSHES THAT HAVE SUIT ABLE VEGETATION IN ANY GIVEN YEAR AS A RESULT OF mUCTU ATIONS IN WATER LEVEL ,ANDUSE CHANGES HAVE GREATLY REDUCED THE AMOUNT OF SUITABLE HABITAT AND FURTHER CHANGES IN WATER LEVELS CAUSED BY INCREASES IN SPRING RAIN OR SUMMER DRYING COULD RENDER REMAINING MARSHES UNUSABLE SEE BOX P &INALLY MOST AQUATIC BIRDS IN THE REGION DEPEND UPON SEASONAL mOOD PULSES AND GRADUAL DROPS IN WATER LEVELS #HANGES IN THE TIMING AND SEVERITY OF THE mOOD PULSE WILL AFFECT THE AVAILABILITY OF SAFE BREED ING SITES FOR BIRDS AND 1 , Ê Ó Ó AMPHIBIANS -IDSUMMER i«>À`ÊÀ}ÊÊ7ÃVÃÊ7iÌ>` hSPIKEv FLOODS FOR EX AMPLE CAN FLOOD BIRD NESTS IN SMALL WETLANDS AND ATTRACT PREDATORS SUCH AS RACCOONS TO AREAS WHERE BIRDS AND AMPHI BIANS BREED #HANGES IN THE TIMING OF THE SPRING MELT ALSO GREATLY ALTER MIGRATORY PATHWAYS AND -iiÊ«>}iÊ{{ TIMING #ANADA GEESE vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi WHICH FORMERLY WINTERED IN mOCKS OF HUNDREDS OF THOUSANDS IN SOUTHERN )LLINOIS NOW MAINLY WINTER IN 7ISCONSIN AND FURTHER NORTH IN )LLINOIS 4HE AVAILABILITY OF SEASONAL MUD mATS FOR MIGRATORY SHOREBIRDS AND ENDANGERED BEACHNESTING SPECIES SUCH AS THE PIPING PLOVER WILL BE AFFECTED BY THE DRYING OR LOSS OF WETLANDS à Ê,iëÃiÃÊÌÊ >ÌiÊ >}i 4 HE BODY TEMPERATURE OF A lSH IS ESSENTIALLY EQUAL TO THE TEMPERATURE OF THE WATER IN WHICH IT LIVES AND EACH SPECIES HAS A CHARAC TERISTIC PREFERRED TEMPERATURE 2ATES OF FOOD CONSUMP TION METABOLISM AND GROWTH RISE SLOWLY AS THE PREFER RED TEMPERATURE IS APPROACHED FROM BELOW AND DROP RAPIDLY AFTER IT IS EXCEEDED UNTIL REACHING ZERO AT THE LETHAL TEMPERATURE #OMMON SPECIES OF lSH CAN BE GROUPED ACCORDING TO THEIR PREFERRED TEMPERATURES INTO hGUILDSv &IGURE &ISH WILL RESPOND STRONGLY TO CHANGES IN WATER VOLUME WATER mOW AND WATER TEMPERATURES EITHER BY SHIFTS IN DISTRIBUTION OR IN OVERALL PRODUCTIVITY >}iÃÊÊà ÊÃÌÀLÕÌ )NDIVIDUAL lSH ACTIVELY SELECT AND RAPIDLY CHANGE LIVING AREAS BASED ON SUITABLE TEMPERATURES OXYGEN CONCENTRATIONS AND FOOD AVAILABILITY #OLDWATER lSH ACTIVELY AVOID TEMPERATURES THAT EXCEED THEIR PREFER RED TEMPERATURE BY TO & TO # DEPENDING ON THE SPECIES AND SEEK OUT REFUGES PROVIDED BY SOURCES OF COOLER WATER SUCH AS GROUNDWATER OR SEEPAGE AREAS AND HEADWATER STREAMS 0HYSICAL CONSTRAINTS SUCH AS DRAINAGE PATTERNS WA TERFALLS AND LANDLOCKED 1 , Ê Ó Î /i«iÀ>ÌÕÀiÊÀÕ«}ÃÊ AREAS PLAY A LARGE ROLE IN vÊ ÊÀi>ÌÊ>iÃÊà DETERMINING THE BOUN DARIES OF A SPECIES RANGE AND THE RATE AT WHICH IT MAY RESPOND TO CHANGING CONDITIONS &OR EXAMPLE TEMPERATURE CONSTRAINTS PREVENTED WHITE PERCH FROM THE !TLANTIC COAST FROM INVADING ,AKE /N TARIO UNTIL THE S 4HEN A SERIES OF WARM -iiÊ«>}iÊ{È WINTERS OVER A YEAR vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA !QUATIC %COSYSTEMS PERIOD PERMITTED THIS SPECIES TO SPREAD THROUGH THE (UDSON 2IVER AND %RIE BARGE CANAL AND INTO ,AKE /NTARIO BY 4ABLE SUMMARIZES THE POTENTIAL IMPACTS OF CLIMATE WARMING ON THE DISTRIBUTION OF lSH SPECIES IN THE 'REAT ,AKES REGION 0OPULATIONS LIVING NEAR THE EDGE OF THE SPECIES RANGE OFTEN EXHIBIT GREATER YEARTOYEAR VARIATION IN ABUN DANCE THAN POPULATIONS LIVING NEAR THE CENTER OF THE RANGE 4HUS WHEN A SOUTHERN BOUNDARY RETRACTS NORTH WARD POPULATIONS WITH HISTORICALLY STABLE ABUNDANCES MAY BECOME MORE VARIABLE 0OPULATIONS LIVING AT THE NORTHERN EDGE OF THE RANGE TEND TO EXHIBIT LOWER GROWTH RATES AND GREATER SENSITIVITY TO EXPLOITATION 4HUS WHEN A NORTHERN BOUNDARY EXTENDS NORTHWARD POPULATIONS NEAR THE OLD BOUNDARY MAY BECOME LESS SENSITIVE TO EXPLOITATION AND EXHIBIT MORE STABLE ABUNDANCE -ANY STUDIES HAVE FORECAST A POTENTIAL NORTHWARD EXPANSION OF THE DISTRIBUTION OF SMALLMOUTH BASS A TYPICAL WARMWATER SPECIES THAT IS NATIVE TO THE SOUTH ERN PART OF THE 'REAT ,AKES BASIN 2ECENT WORK INDICATES THAT THE CONSEQUENCES OF THAT EXPANSION COULD INCLUDE LOCAL EXTIRPATION OF MANY NATIVE MIN NOWS AND NEGATIVE IMPACTS ON NATIVE TOP PREDATORS PARTICULARLY LAKE TROUT IN NEWLY INVADED LAKES 4HESE lNDINGS CLEARLY DEMONSTRATE THE ECOLOGICAL DISRUPTIONS THAT WILL OCCUR THROUGHOUT THE REGION AS COLDWATER SPECIES DISAPPEAR AND WARM AND COOLWATER SPECIES VIE TO TAKE THEIR PLACE IN A WARMER WORLD 4HESE DISRUPTIONS ARE LIKELY TO BE COMPOUNDED BY INVASIONS OF NONNATIVE ORGANISMS MANY OF WHICH ARE CAPABLE OF TOTALLY RESTRUCTURING EXISTING FOOD CHAINS AND CAUSING SIGNIlCANT CONSEQUENCES FOR NATIVE lSH COMMUNITIES 4HE ZEBRA MUSSEL AND %UROPEAN CARP INVASIONS IN THE 'REAT ,AKES REGION ARE PERHAPS THE BEST EXAMPLES OF SUCH MAJOR DISRUPTIVE EVENTS #LIMATE WARMING IS LIKELY TO PERMIT ZEBRA MUSSELS AND COM MON CARP TO EXPAND THEIR EXISTING RANGES NORTHWARD IN THE 'REAT ,AKES REGION !S NOTED EARLIER HIGHER SUMMER SURFACE WATER TEMPERATURES AND INCREASED SUMMER ANOXIA IN DEEPER WATERS MAY LEAD TO GREATER RELEASE OF MERCURY FROM SEDIMENTS 4HAT WOULD LEAD TO HIGHER MERCURY LEVELS IN lSH WHICH WOULD HARM NOT ONLY lSH POPULATIONS BUT HUMAN CONSUMERS AS WELL /ÊÈÊÊÊ >}iÃÊ"LÃiÀÛi`]Ê*Ài`VÌi`]Ê>`Ê*ÃÃLiÊÊÌ iÊ,>}iÃÊ ÊÊvÊà Ê-«iViÃÊÊÌ iÊ>iÃÊ>`Ê,ÛiÀÃÊvÊÌ iÊÀi>ÌÊ>iÃÊ>à ÃÌÀLÕÌ>Ê >}ià «>VÌÃÊÊ-«iVià ÝÌiÃÊ>ÌÊ ÀÌ iÀÊÌ *iÀV ]ÊÃ>ÕÌ ÊL>ÃÃ\Ê*Ài`VÌi`ÊÎääiÊiÝÌiÃÊvÊiÝÃÌ}ÊLÕ`>ÀÞÊ >VÀÃÃÊ >>`>ÊÜÌ ÊÇcÊVÀi>ÃiÊÊi>Ê>Õ>Ê>ÀÊÌi«iÀ>ÌÕÀi> ->ÕÌ ÊL>ÃÃ]ÊV>À«\Ê*Ài`VÌi`ÊÎääiÊiÝÌiÃÊvÊiÝÃÌ}ÊLÕ`>ÀÞÊ Ê"Ì>ÀÊÜÌ ÊcÊVÀi>ÃiÊÊi>Ê>Õ>Ê>ÀÊÌi«iÀ>ÌÕÀiL ÜÃÊ­nÊëiViî]ÊÃÕwÊà iÃÊ­ÇÊëiViî]ÊÃÕViÀÃÊ­ÎÊëiViî]ÊÌ«ÜÃÊ ­ÎÊëiViî\Ê*Ài`VÌi`ÊiÝÌiÃÊÌÊÀi>ÌÊ>iÃÊL>ÃÊ«ÃÃLiÊÜÌ ÊÜ>À}V ,iÌÀ>VÌÊ>ÌÊ ÃÕÌ iÀÊÌ 7 ÌiwÊà ]ÊÀÌ iÀÊ«i]ÊÜ>iÞi\Ê*Ài`VÌi`ÊÀiÌÀ>VÌÊLiV>ÕÃiÊvÊÀÌ Ü>À`Ê Ã vÌÊÊÃÕÃÌ>>LiÊÞi`ÃÊiÝ«iVÌi`ÊÌÊÀiÃÕÌÊvÀÊV>ÌiÊV >}i` >iÊÌÀÕÌÊ>`ÊÌ iÀÊV`Ü>ÌiÀÊëiViÃ\Ê,iÌÀ>VÌÊ«Ài`VÌi`ÊÊÃ>Êà i`Ê>iÃÊ >ÌÊÃÕÌ iÀÊÌÊLiV>ÕÃiÊÜiÀÊ"ÓÊiÛiÃÊÜÊà ÀÊ`ii«Ü>ÌiÀÊÀivÕ}iÃÊvÀÊ «Ài`>ÌÊÊÃÕiÀi ÀÊÌÀÕÌ\Ê,iÌÀ>VÌÊ«Ài`VÌi`ÊvÀÊÃÌÀi>ÃÊ>ÌÊÜiÀÊiiÛ>ÌÃÊÌ ÀÕ} ÕÌÊ Ì iÊÃÕÌ iÀÊi`}iÊvÊÌ iÊÀ>}iÊLiV>ÕÃiÊvÊiÝ«iVÌi`ÊVÀi>ÃiÃÊÊ}ÀÕ`Ü>ÌiÀÊ Ìi«iÀ>ÌÕÀiÃv >ÀÀiÀÊÀii>ÃiÊ>`Ê À>}iÊiÝ«>à 7 ÌiÊ«iÀV \Ê"LÃiÀÛi`ÊÛ>ÃÊ>`ÊëÀi>`ÊÌ ÀÕ} ÊÀi>ÌÊ>iÃÊL>ÃÊÜ iÊ£{äÃÊ Ü>À}ÊvÊÕ`ÃÊ,ÛiÀÊ>`ÊÀiÊL>À}iÊV>>ÊÜ>ÌiÀÃÊivviVÌÛiÞÊÀiÛi`ÊÌ iÀ>Ê L>ÀÀiÀÊ>`Ê«iÀÌÌi`Ê>VViÃÃ} -ÌÀ«i`ÊL>ÃÃ\Ê*Ài`VÌÃÊ`V>ÌiÊÌ >ÌÊÜ>À}Ê>ÞÊ«iÀÌÊÌ ÃÊëiViÃÊÌÊÛ>`iÊ Ì iÊÀi>ÌÊ>iÃÊL>ÃÊ>`ÊÌ ÕÃÊiÝ«>`ÊÌÃÊÀ>}iÊi>ÃÌÜ>À` -ÕÀViÃ\Ê-iiÊÌiÊ£Ó£° # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA >}iÃÊÊà Ê*À`ÕVÌÛÌÞ 7ITHIN A LAKE THE PRODUCTIVITY OF A lSH POPULATION IS RELATED TO THE AMOUNT OF SUITABLE LIVING SPACE THAT IS THE VOLUME OF THERMALLY SUITABLE WATER 3TUDIES OF WALLEYE LAKE TROUT AND WHITElSH HAVE DEMONSTRATED THAT THE ABUNDANCE AND PRODUCTIVITY OF lSH INCREASE WITH INCREASED TIME SPENT AT THE OPTIMAL TEMPERATURE 4HERE IS ALSO A TRADEOFF BETWEEN THE POSITIVE EFFECT OF WARMER TEMPERATURES ON lSH PRODUCTION AND THE NEGA TIVE EFFECT OF LOWER LAKE LEVELS DUE TO DRYING &OR EXAMPLE GIVEN A SCENARIO WHERE ANNUAL AIR TEMPERA TURE RISES & # AND LAKE DEPTH DROPS FEET DATA FROM .ORTH !MERICAN LAKES SUGGEST THAT lSH PRODUC TION WILL DECREASE IN LAKES WITH A MEAN DEPTH OF FEET OR LESS AND INCREASE IN LAKES WITH A MEAN DEPTH GREATER THAN FEET 0RODUCTION OF SEVERAL SPECIES OF SPORT lSH LAKE TROUT WALLEYE AND PIKE AND COMMERCIALLY HARVESTED lSH WHITElSH IN THE REGION CURRENTLY VARIES WITH THE AMOUNT OF THERMALLY SUITABLE HABITAT &IGURE 0REDICTIONS ARE THAT CLIMATE WARMING WILL GREATLY REDUCE THE AMOUNT OF THERMALLY SUITABLE HABITAT FOR LAKE TROUT IN MANY INLAND LAKES 4HIS WOULD EFFEC TIVELY ELIMINATE LAKE TROUT FROM ALMOST ALL SHALLOW LAKES IN THE REGION BECAUSE OF hSUMMERKILLv A LETHAL COMBINATION OF HIGH SURFACE WATER TEMPERATURES AND DECREASED OXYGEN IN BOTTOM WATERS 4HIS FORECAST IS CONSISTENT WITH EARLIER WORK THAT PREDICTED COLDWATER lSH LIVING IN LARGE COLD 1 , Ê Ó { LAKES WILL BE THE MOST 7>ÌiÀÊ/i«iÀ>ÌÕÀiÊ SECURE AGAINST THE NEGA >`Êà ÊÃÌÀLÕÌÊ >}ià TIVE IMPACTS OF CLIMATE CHANGE )N CONTRAST OTHER STU DIES PREDICT LESS WINTERKILL OF WARM AND COOLWATER FISH LIVING IN SHALLOW INLAND LAKES BECAUSE SHORTER PERIODS OF ICE COVER WOULD ELIMINATE WINTER OXYGEN DElCITS -OST NORTHERN LAKES ARE -iiÊ«>}iÊ{È LIKELY TO DEVELOP MORE vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi SUITABLE TEMPERATURES FOR WALLEYE A TYPICAL COOLWATER SPECIES IN /NTARIO (OWEVER A FEW SOUTHERN LAKES ARE LIKELY TO BECOME LESS SUITABLE WITH SUMMER TEMPERATURES REACHING LEVELS TOO WARM FOR OPTIMAL GROWTH VVÊ ÃiµÕiViÃÊvÊ >ÌiÊ >`ÊV}V>Ê >}iÊʵÕ>ÌVÊ-ÞÃÌià 7>ÌiÀÊiÛiÃ]Ê- ««}]Ê >`ÊÞ`À«ÜiÀÊiiÀ>Ì ECREASES IN WATER LEVELS HAVE BROAD IMPLICA TIONS FOR BOTH ECOLOGICAL AND HUMAN SYSTEMS IN AND AROUND THE LARGE LAKES 3HIP CLEAR ANCE IN CHANNELS AND HARBORS IS REDUCED REQUIRING SHIPS TO CARRY LESS WEIGHT IN ORDER TO RIDE HIGHER IN THE WATER 4HE 'REAT ,AKES #ARRIERS !SSOCIATION ESTI MATES THAT WITH A ONEINCH DROP IN LAKE LEVEL A FOOT SHIP LOSES TONS OF CARGO CAPACITY !N EARLIER ASSESSMENT BASED ON MILDER PROJECTIONS OF WARMING FOUND THAT SHIPPING COSTS COULD INCREASE BY TO PERCENT AS A RESULT OF LOWER LAKE LEVELS ! POTENTIAL COUNTER TO THIS NEGATIVE IMPACT IS THAT REDUCED ICE COVER WILL LENGTHEN THE SHIPPING SEASON ON THE 'REAT ,AKES 3TEPPEDUP DREDGING OF CHANNELS AND HARBORS IS OFTEN USED TO INCREASE SHIP CLEARANCE IN TIMES OF LOW WATER INCURRING BOTH DIRECT ECONOMIC COSTS AND $ ENVIRONMENTAL COSTS 4HE DIRECT COSTS OF DREDGING COULD EXCEED MILLION 53 ANNUALLY "UT DREDGING OFTEN STIRS UP BURIED POLLUTANTS WHICH MAY IMPOSE ADDITIONAL COSTS ON SOCIETY 4HE ESTIMATED COSTS FOR A FOUR TO EIGHTFOOT DROP IN WATER LEVEL RANGE FROM MILLION TO MILLION 53 AND THE PRICE FOR EXTENDING WATER SUPPLY PIPES DOCKS AND STORMWATER OUTFALLS TO THE NEW WATERLINE WOULD ADD ANOTHER MILLION TO MILLION 53 $ECREASED WATER LEVELS COULD REDUCE HYDROPOWER GENERATION BY AS MUCH AS PERCENT BY AN ES TIMATE THAT IS LIKELY TO BE CONSERVATIVE BECAUSE IT WAS BASED ON OLDER CLIMATE MODELS (YDROPOWER ACCOUNTS FOR ALMOST PERCENT OF THE ELECTRICITY GENERATED IN /NTARIO WHILE IN THE 5NITED 3TATES SIGNIlCANT HYDROPOWER IS GENERATED AT THE -OSES .IAGARA 0LANT IN .EW 9ORK 3TATE &IGURE $EMAND FOR MORE HYDROPOWER WILL BE CREATED IN THE FUTURE BY THE NEED # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA !QUATIC %COSYSTEMS /ÊÇÊÊÊ >ÌiÊ >}iÊ«>VÌÃÊÊà ÊV}ÞÊ>`Ê ÃiµÕiViÃÊvÀÊà iÀià >ÌiÊ >}iÊ«>VÌÃÊÊà ÊV}ÞÊ ÃiµÕiViÃÊvÀÊà iÀià >}iÊÊÛiÀ>ÊwÊà ʫÀ`ÕVÌÊÊ>Ê«>ÀÌVÕ>ÀÊ >µÕ>ÌVÊiVÃÞÃÌiÊ >}iÊÊÃÕÃÌ>>LiÊ >ÀÛiÃÌÃÊvÀÊ>ÊwÊà ʫ«Õ>ÌÃÊ ÊÌ iÊiVÃÞÃÌi >}iÊÊÀi>ÌÛiÊ«À`ÕVÌÛÌÞÊvÊ`Û`Õ>ÊwÊÃ Ê ««Õ>ÌÃÊÊ>Ê«>ÀÌVÕ>ÀÊ>µÕ>ÌVÊiVÃÞÃÌi >}iÊÊÌ iÊÀi>ÌÛiÊiÛiÃÊvÊiÝ«Ì>ÌÊÌ >ÌÊV>Ê LiÊÃÕÃÌ>>LÞÊ`ÀiVÌi`Ê>}>ÃÌÊÌ iÊwÊà ʫ«Õ>ÌÃÊ vÊÌ iÊiVÃÞÃÌiÊ >À}iÃV>iÊà vÌÃÊÊ}i}À>« VÊ`ÃÌÀLÕÌÊ vÊëiVià >}iÊÊÝÌÕÀiÊvÊëiViÃÊÌ >ÌÊV>ÊLiÊÃÕÃÌ>>LÞÊ >ÀÛiÃÌi`ÊÜÌ Ê>ÊëiVwÊVÊ}i}À>« VÊ>Ài> >}iÊÊV>ÌÊvÊ«ÀwÊÌ>LiÊwÊà }Ê}ÀÕ`à ->ÃV>iÊà vÌÃÊÊÌ iÊë>Ì>Ê`ÃÌÀLÕÌÊ vÊiLiÀÃÊvÊ>ÊëiVwÊVÊ««Õ>ÌÊ TO REDUCE #/ EMISSIONS FROM FOSSIL FUELlRED POWER PLANTS !S HYDROPOWER OPPORTUNITIES DECLINE IN THE 'REAT ,AKES REGION PRESSURE MAY INCREASE TO BUILD SUCH PROJECTS ELSEWHERE SUCH AS IN THE *AMES "AY REGION 7ATER WITHDRAWALS FROM THE 'REAT ,AKES ARE 1,ÊÓx ALREADY SUBJECT TO CONTEN 7>ÌiÀÊ >}iÃÊvviVÌÊÞ`À«ÜiÀ TIOUS DEBATE AND POLITICAL LEADERS IN THE REGION HAVE OPPOSED FURTHER WITHDRAW ALS ESPECIALLY FOR WATER TO BE SHIPPED OUT OF THE BASIN 'IVEN PROJECTIONS FOR DRIER SUMMERS IN THE REGION PRESSURE TO INCREASE WATER EXTRACTION FOR IRRIGATION DRINKING AND OTHER USES -iiÊ«>}iÊ{Ç WILL GROW EVEN WITHIN THE vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi BASIN /NE STUDY FOUND THAT THE SYNERGISTIC EFFECTS OF PREDICTED DECREASES IN RUNOFF AND INCREASES IN IRRIGATION COULD BE DEVASTATING TO THE REGIONS STREAMS à iÀià #LIMATEDRIVEN CHANGES IN lSH POPULATIONS AND COM MUNITIES WILL PRODUCE A VARIETY OF IMPACTS ON EXISTING lSHERIES 4ABLE -OST OF THESE IMPACTS WILL STEM FROM TWO MECHANISMS THE SUSTAINABLE HARVEST OF lSH WILL RISE AND FALL WITH SHIFTS IN OVERALL AQUATIC PRODUCTIVITY AND SUSTAINABLE HARVESTS FROM A >}iÊÊÃÕÃÌ>>LiÊ >ÀÛiÃÌÊvÀÊÌ iÊ««Õ>Ì >}iÊÊivwÊViVÞÊvÊwÊà }Ê}i>À]Êi>`}ÊÌÊV >}iÊ ÊÃÕÃÌ>>LiÊiÛiÃÊvÊwÊà }ÊivvÀÌ SPECIlC POPULATION IN A SPECIlC LOCATION MAY INCREASE SUBSTANTIALLY OR FALL TO ZERO DEPENDING ON HOW NEW CLIMATE CONDITIONS AND SPECIESSPECIlC TEMPERATURE NEEDS INTERACT 4HE COMMERCIAL lSHING SECTOR IN THE REGION IS RELA TIVELY SMALL ,ANDED CATCHES IN THE LATE S WERE VALUED AT ABOUT MILLION 53 INCLUDING MIL LION TAKEN BY #ANADIAN lSHERS AND MILLION TAKEN BY 53 lSHERS -OST OF THE COMMERCIAL CATCH IN #ANADA COMES FROM ,AKE %RIE AND THAT IN THE 5NITED 3TATES FROM ,AKE -ICHIGAN )N CONTRAST THE RECREATIONAL lSHING SECTOR IS QUITE LARGE IN BOTH COUNTRIES )N THE S MILLION RECREATIONAL ANGLERS SPENT BILLION 53 ON lSHING IN 53 WATERS AND MILLION ANGLERS SPENT BILLION #DN ON lSHING IN #ANADIAN WATERS 4HESE ANGLERS SPENT ABOUT MILLION lSHING DAYS ON THE 'REAT ,AKES ALONE NOT COUNTING lSHING ON INLAND LAKES RIVERS AND STREAMS ,ARGE CHANGES IN THE DISTRIBUTION AND PRODUCTIVITY OF lSH SPECIES IN THE REGION WILL SIGNIl CANTLY IMPACT THE NEARLY MILLION ANGLERS THAT ACTIVELY lSH THESE WATERS 4HESE DOLLAR lGURES DO NOT REmECT THE FULL VALUE OF CEREMONIAL AND ARTISANAL lSHERIES PRACTICED BY .ATIVE !MERICANS AND &IRST .ATIONS IN MANY SETTLEMENTS SCAT TERED THROUGHOUT THE 'REAT ,AKES BASIN &ISHING PLAYS AN IMPORTANT ROLE IN THE TRADITIONAL SOCIAL STRUCTURES OF THESE COMMUNITIES A ROLE THAT DElES EASY QUANTI lCATION AND WILL NOT BE REmECTED IN COST ACCOUNTINGS OF IMPACTS THAT ARE BASED PURELY ON MARKET MEASURES # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA #(!04%2 &OUR %COLOGICAL 6ULNERABILITY TO #LIMATE #HANGE 4ERRESTRIAL %COSYSTEMS ÀiÃÌi`Ê>`ÃV>«ià 4 HE DISTRIBUTION OF FOREST TYPES IN THE 'REAT ,AKES REGION IS CONTROLLED BY A PATTERN OF IN CREASING RAINFALL AS ONE MOVES FROM WEST TO EAST AND COLDER TEMPERATURE AS ONE MOVES SOUTH TO NORTH 4HESE CLIMATIC GRADIENTS GAVE RISE TO FORESTS DOMINATED BY OAKS AND HICKORIES IN THE SOUTHERN 'REAT ,AKES REGION NORTHERN HARDWOOD FORESTS COMPOSED OF SUGAR MAPLE !MERICAN BEECH AND !MERICAN BASS WOOD FARTHER NORTH AND BOREAL FORESTS DOMINATED BY WHITE SPRUCE AND BALSAM lR IN THE NORTHERNMOST PORTION OF THE REGION &IGURE )N THE DRIER WESTERN PART OF THE REGION CLOSED CANOPY FORESTS GIVE WAY TO SCATTERED SAVANNAS CONSISTING OF BUR OAK AND MIXED PRAIRIE GRASSES (UMAN LANDUSE DECISIONS HAVE RESHAPED MUCH OF WHAT CLIMATE SOILS AND GEOLOGY WROUGHT /N DROUGHT PRONE SOILS FREQUENT WILDlRES ONCE MAINTAINED CONIF EROUS FORESTS COMPOSED OF WHITE AND RED PINE IN THE NORTHERN PORTION OF THE REGION 4HESE WERE LARGELY ELIMINATED BY INTENSIVE TIMBER HARVESTS DURING THE LATE S )N THE SOUTHERN 'REAT ,AKES REGION LARGE AREAS OF FERTILE SOILS ONCE IN FOREST COVER HAVE BEEN IN AGRICULTURAL PRODUCTION FOR ALMOST YEARS -AJOR AREAS STILL DOMINATED BY FORESTS LIE MOSTLY IN THE NORTHERN PARTS OF -ICHIGAN -INNESOTA AND 7ISCON SIN AND IN /NTARIO WHERE CLIMATIC AND SOIL CONDITIONS ARE LESS FAVORABLE FOR AGRICULTURE &ORESTS CURRENTLY OCCUPY PERCENT OF THE TOTAL LAND AREA IN THE 53 'REAT ,AKES STATES AND PERCENT OF THE LAND AREA IN /NTARIO ÃÌÀLÕÌÊ>`Ê*À`ÕVÌÛÌÞ 4REE SPECIES HAVE BEEN MIGRATING ACROSS THE REGION IN RESPONSE TO CLIMATE CHANGE SINCE THE END OF THE LAST ICE AGE SOME YEARS AGO 4HE PACE OF CLIMATE CHANGE WILL ACCELERATE OVER THE NEXT CENTURY HOWEVER AND THE ABILITY OF FOREST TREES TO MIGRATE IN RESPONSE WILL DEPEND NOT ONLY ON THEIR OWN TRAITS SUCH AS WHETHER THEIR SEEDS ARE DISPERSED ON THE WIND OR BY ANIMALS AND NATURAL GEOGRAPHIC BARRIERS SUCH AS THE 'REAT ,AKES BUT ALSO ON HUMAN LANDUSE DECISIONS 'EOGRAPHIC VARIATION IN 1,ÊÓÈ SOIL MOISTURE AND TEXTURE / iÊ ÀÌ iÀÊÀiÃÌà WILL ALSO PUT STRONG CON STRAINTS ON THE MOVEMENT OF PLANT SPECIES AND THE COMPOSITION OF FUTURE FORESTS IN ANY GIVEN LOCA TION 7ARMER TEMPERA TURES AND A LONGER GROW ING SEASON ARE LIKELY TO RESULT IN THE NORTHWARD -iiÊ«>}iÊ{n MOVEMENT OF MANY FOREST vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 4E R R E S T R I A L % C O S Y S T E M S SPECIES AND A GENERAL DECLINE IN THE EXTENT OF BOREAL NUTRIENTPOOR SOIL %LEVATED #/ COULD ALSO ACCEL FORESTS IN THE REGION .ORTHERN CONIFERS SUCH AS ERATE THE PACE OF FOREST SUCCESSION SPEEDING UP THE WHITE PINE AND HEMLOCK ARE LIKELY TO BE RESTRICTED TO RATE AT WHICH hPIONEER SPECIESv SUCH AS ASPEN WHICH ISOLATED POPULATIONS OR LOST COMPLETELY FROM SOUTHERN COLONIZE SITES FOLLOWING DISTURBANCES SUCH AS TIMBER )LLINOIS )NDIANA AND /HIO 4REE AND PRAIRIE GRASS HARVESTING OR lRE GIVE WAY TO SPECIES SUCH AS MAPLE SPECIES IN THE WESTERN PART OF THE REGION ARE LIKELY THAT ESTABLISH IN THE SHADE OF THE PIONEERING TREES TO MOVE EASTWARD ESPECIALLY IF WARMER TEMPERATURES -APLE TREES GROWN UNDER ELEVATED #/ BECOME MORE RESULT IN MORE FREQUENT DRYING OUT OF SOILS OR EVEN TOLERANT OF SHADE AND INCREASE THEIR GROWTH RATE &ASTER DROUGHTS IN THEIR CURRENT RANGE FOREST DEVELOPMENT COULD SHORTEN THE HARVEST ROTATION 0RIOR TO WIDESPREAD lRESUPPRESSION EFFORTS DUR FOR ASPEN MANAGED FOR lBER PRODUCTION IN THE NORTHERN ING THE TWENTIETH CENTURY lRE WAS AN IMPORTANT AGENT PARTS OF THE REGION SHAPING THE COMPOSITION AND DISTRIBUTION OF FORESTS !NOTHER FACTOR THAT COULD BOOST FOREST GROWTH AND IN THE REGION &IRES SWEPT THROUGH THE NORTHERN PRODUCTIVITY IS THE AVAILABILITY OF NITROGEN A KEY PLANT FORESTS EVERY TO YEARS MAINTAINING NEARLY NUTRIENT (UMAN ACTIVITIES INCLUDING THE FOSSIL FUEL PERCENT OF THE LAND AREA AS YOUNG RECENTLY BURNED BURNING THAT IS HELPING TO DRIVE CLIMATE CHANGE HAVE FOREST STANDS 3URFACE lRES THAT CONSUMED DEAD LEAVES ALMOST DOUBLED THE AMOUNT OF NITROGEN ENTERING FORESTS AND TWIGS LYING ON THE GROUND WERE COMMON IN VIA RAIN SNOW AND DRY AIRBORNE PARTICLES -UCH OF HARDWOOD FORESTS GROWING ON MOIST SOILS WHEREAS THE EXCESS NITROGEN FALLING ON FORESTS IS DEPOSITED AS SEVERE CANOPYCONSUMING lRE OFTEN NITRATE WHICH IS RAPIDLY TAKEN UP BY DESTROYED RED AND JACK PINE FOREST ON SOIL MICROORGANISMS AND EVENTUALLY ÀiÃÌÊ}ÀÜÌ ÊVÕ`Ê DRY SANDY SOIL &IRE HISTORY STUDIES MADE AVAILABLE TO FERTILIZE PLANT HAVE SHOWN THAT OVER THE PAST GROWTH )N THIS WAY FORESTS FUNC «ÌiÌ>ÞÊ}iÌÊ>Ê YEARS lRE WAS MORE FREQUENT DURING TION AS hLIVING lLTERSv PREVENTING LÃÌÊvÀÊÌ iÊÀÃiÊ PERIODS OF WARM TEMPERATURES AND NITRATE FROM LEACHING INTO GROUND LOW PRECIPITATION WHICH SUGGESTS Ê>Ìë iÀVÊ "Ó° WATER STREAMS AND LAKES WHERE IT FOREST lRE FREQUENCY IS LIKELY TO IN BECOMES A POLLUTANT 4HIS lLTERING CREASE AS THE CLIMATE TURNS WARMER AND CAPACITY MAY BE EXCEEDED IN THE LONG SUMMERS BECOME DRIER )N FACT AS A RESULT OF THE TERM BUT IN THE SHORT TERM EXTRA NITROGEN FROM THE PROJECTED HIGHER TEMPERATURES AND LOWER SUMMER ATMOSPHERE COULD ENHANCE THE ABILITY OF FOREST TREES PRECIPITATION MODELS SUGGEST DECREASED SOIL MOISTURE TO GROW FASTER IN RESPONSE TO RISING ATMOSPHERIC #/ DURING SUMMER AND AUTUMN WHICH WOULD NOT ONLY /ZONE HOWEVER MAY COUNTER THE GROWTHENHANC INCREASE THE lRE RISK BUT ALSO LIMIT FOREST GROWTH IN ING POTENTIAL OF BOTH #/ AND NITROGEN 'ROUNDLEVEL DRIER AREAS FOR MORE WEEKS PER SUMMER )N WETTER CONCENTRATIONS OF OZONE ARE INCREASING ESPECIALLY AREAS FOREST GROWTH IS RARELY WATER LIMITED 4HE DOWNWIND OF MAJOR URBAN AREAS IN THE REGION %LEV RESPONSE TO CHANGING SOIL MOISTURE WILL ALSO INTERACT ATED OZONE CONCENTRATIONS CAN DAMAGE TREE LEAVES WITH CHANGES IN lRE FREQUENCY SINCE FORESTS IN DRIER DAMPING GROWTH AND RENDERING TREES MORE VULNERABLE AREAS ARE MORE lREPRONE TO INSECT PESTS AND DISEASES 3USCEPTIBILITY TO OZONE &OREST GROWTH COULD POTENTIALLY GET A BOOST FROM DAMAGE VARIES AMONG TREE SPECIES AND ALSO AMONG THE RISE IN ATMOSPHERIC #/ THAT IS HELPING TO DRIVE DIFFERENT INDIVIDUALS WITHIN A SPECIES %XPERIMENTS CLIMATE CHANGE #/ ACTS AS A PLANT FERTILIZER AND THAT EXPOSED YOUNG ASPEN PAPER BIRCH AND SUGAR NATIVE TREES GROWN EXPERIMENTALLY IN ELEVATED #/ MAPLE TO BOTH #/ AND OZONE INDICATE THAT RELATIVELY HAVE SHOWN INCREASED GROWTH 4REMBLING ASPEN AN SMALL INCREASES IN OZONE CAN ELIMINATE THE GROWTH ECOLOGICALLY AND ECONOMICALLY IMPORTANT TREE IN THE ENHANCING EFFECTS OF ELEVATED #/ REGION COULD INCREASE ITS GROWTH TO PERCENT AS .O ONE CAN YET PREDICT EXACTLY HOW CHANGES IN #/ LEVELS RISE !SPEN FORESTS ON FERTILE SOIL WILL EXPERI TEMPERATURE MOISTURE lRE #/ NITROGEN AND OZONE ENCE GREATER GROWTH ENHANCEMENT THAN THOSE ON WILL INTERACT OVER THE COMING DECADES TO ALTER THE &OR ADDITIONAL CLIMATE MODELING RESULTS AND OTHER TECHNICAL INFORMATION SEE WWWUCSUSAORGGREATLAKES # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA GROWTH AND DISTRIBUTION OF FORESTS 4HE UNCERTAINTY STEMS IN PART FROM THE CENTURIESLONG LIFESPAN OF FOREST TREES %VEN MULTIYEAR EXPERIMENTS SUBJECTING SAPLINGS TO ENHANCED LEVELS OF #/ CANNOT DETERMINE FOR EXAMPLE WHETHER THE FASTER GROWTH MEANS TREES WILL ACTUALLY GROW LARGER OR WILL SIMPLY REACH THE SAME SIZE FASTER THAN TREES GROWING AT CURRENT #/ LEVELS !ND NO STUDIES HAVE ATTEMPTED TO LOOK AT ALL THE INTERACT ING HUMAN AND ENVIRONMENTAL FACTORS THAT WILL SHAPE THE FATE OF FUTURE FORESTS IN THE 'REAT ,AKES REGION «>VÌÃÊÊÀiÃÌÊÃiVÌà )NSECTS HAVE THE POTENTIAL TO SHIFT BOTH THE MAGNITUDE AND DIRECTION OF PLANT RESPONSES TO CLIMATE CHANGE 4HROUGH THEIR ROLES AS HERBIVORES POLLINATORS AND DECOMPOSERS INSECTS INmUENCE PRIMARY PRODUCTION COMMUNITY COMPOSITION NUTRIENT CYCLING AND SUC CESSIONAL PROCESSES IN THE FORESTS 4HE FATE OF ANY PAR TICULAR INSECT SPECIES IN A CHANGED CLIMATE IS DIFlCULT TO PREDICT YET SOME GENERAL TRENDS CAN BE FORESEEN 4HE NORTHERN LIMIT OF SOME DEVASTATING FOREST PESTS SUCH AS THE GYPSY MOTH IS CURRENTLY DETERMINED BY COLD WINTER TEMPERATURES AND THESE INSECTS WILL ALMOST CERTAINLY BECOME MORE WIDELY ESTABLISHED THROUGHOUT THE REGION IN A WARMER CLIMATE &IGURE )NSECT RANGES MAY ALSO SHIFT AS THEIR HOST TREES MIGRATE IN RESPONSE TO CLIMATE &OR EXAMPLE THE RANGE OF THE EASTERN TIGER SWALLOWTAIL IS LIKELY TO EXPAND NORTHWARD COINCIDENT WITH EXPANSION OF THE RANGE OF ITS PREFERRED HOST THE TULIP TREE 3IMULTANEOUSLY THE RANGE OF THE #ANADIAN TIGER SWALLOWTAIL WILL RETRACT NORTHWARD AS ITS PREFERRED HOST ASPEN DISAPPEARS FROM THE SOUTHERN 'REAT ,AKES REGION &IGURE #LIMATIC CHANGES THAT ALTER THE SYNCHRONY BETWEEN KEY INSECTS DESIRABLE AND UNDESIRABLE AND THEIR HOST PLANTS COULD MARKEDLY AFFECT FOREST ECOSYSTEMS 3EVERAL OF THE MOST DAMAGING PESTS IN THE REGION SUCH AS THE FOREST TENT CATERPILLAR GYPSY MOTH AND SPRUCE BUD WORM ARE SPRINGFEEDING INSECTS WHOSE EMERGENCE IS CLOSELY SYNCHRONIZED WITH THE BUDBREAK OF THEIR HOSTS !LTHOUGH BOTH INSECT EMERGENCE AND BUDBREAK ARE CONTROLLED BY TEMPERATURE IT IS UNCLEAR WHETHER CLIMATE WARMING WILL ALTER BOTH PROCESSES AT THE SAME RATE !SYNCHRONY BY AS LITTLE AS A WEEK COULD MARKEDLY ALTER INSECT lTNESS AND THE POTENTIAL FOR OUTBREAKS 4HE ACTIVITY OF INSECT PREDATORS AND PARASITOIDS THAT PREY ON INSECT PESTS IS ALSO CONTROLLED BY TEMPERATURE AND HOW WARMER CLIMATES WILL ALTER THEIR EFFECTIVENESS AS NATURAL ENEMIES IS VIRTUALLY UNKNOWN 0OLLINATION SERVICES ARE ANOTHER CRITICAL INSECTPLANT INTERACTION THAT COULD BE DISRUPTED IF CLIMATE CHANGE DECOUPLES THE TIMING OF mOWERING AND POLLINATOR ACTIVITY )N ADDITION TO CLIMATE CHANGES BOTH ELEVATED ATMOSPHERIC #/ AND 1,ÊÓÇ ELEVATED OZONE ARE LIKE ÀiÃÌÊ*iÃÌÃÊÊ>Ê >}}Ê >Ìi LY TO AFFECT INSECTS VIA CHANGES IN HOST QUALITY 4HE LEAVES OF PLANTS GROWN UNDER ENRICHED #/ TYPICALLY ARE RE DUCED IN FOOD VALUE THAT IS LOWER IN PROTEIN AND HIGHER IN UNPALATABLE COMPOUNDS SUCH AS TAN NINS ,EAFCHEWING -iiÊ«>}iÊ{Ç INSECTS FED THIS MATERIAL vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi GENERALLY EAT MORE TO COMPENSATE FOR LOW PRO 1 , Ê Ó n ,>}iÊ- vÌÃÊvÊÌ iÊ TEIN LEVELS 4HEY ALSO >>`>Ê/}iÀÊ-Ü>ÜÌ> EXPERIENCE SLOWER DEVEL OPMENT AND REDUCED GROWTH EFFICIENCY 7HETHER THIS PHENOM ENON WILL RESULT IN GREATER DEFOLIATION OF FORESTS IS UNKNOWN BECAUSE AL THOUGH INDIVIDUAL INSECTS MAY EAT MORE OVERALL INSECT POPULATION DENSI TIES MIGHT DECLINE %LEV -iiÊ«>}iÊ{n vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi ATED OZONE CONCENTRA TIONS IN THE LOWER ATMOSPHERE CAN ALSO CHANGE PLANT CHEMISTRY )N TREMBLING ASPEN OZONE EXPOSURE COM PROMISES PRODUCTION OF THE MAJOR CHEMICAL DEFENSE COMPOUNDS LEADING TO IMPROVED PERFORMANCE BY FOREST TENT CATERPILLARS $ESPITE NUMEROUS UNCERTAINTIES IT IS CLEAR THAT COMING CHANGES WILL NOT AFFECT ALL PLANTS INSECTS AND THEIR NATURAL ENEMIES UNIFORMLY 4HE lTNESS OF SOME WILL IMPROVE WHILE THAT OF OTHERS WILL DETERIORATE 3HIFTS IN INSECT POPULATION AND COMMUNITY DYNAMICS WILL FEED BACK TO AFFECT HOW FORESTS OF THE REGION FUNCTION AS RESPONDERS TO AND MODULATORS OF CLIMATE CHANGE # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 4E R R E S T R I A L % C O S Y S T E M S ARE MOST ABUNDANT IN ASPEN FORESTS MIGHT BE ESPE «>VÌÃÊÊ7`vi CIALLY LIKELY TO SHIFT THEIR RANGES TO THE NORTH )NDEED /NE IMPORTANT ECOLOGICAL IMPLICATION OF FOREST CHANGE THE FAILURE OF EFFORTS TO REINTRODUCE RUFFED GROUSE TO IS THE POSSIBLE DEGRADATION OF MIGRATORY CORRIDORS FOR PARTS OF THEIR HISTORICAL RANGE IN )LLINOIS MIGHT BE ANIMALS ! WIDE GAP OF LARGELY AGRICULTURAL LANDS EXISTS PARTLY A RESULT OF CHANGING FOREST CONDITIONS CAUSED BETWEEN THE EXTENSIVE TROPICAL FORESTS OF #ENTRAL AND BY CLIMATE CHANGE AS WELL AS HUMAN LAND USE 3OUTH !MERICA AND FORESTS IN THE NORTHERN 'REAT ,AKES #LIMATE WARMING MAY ALSO BENElT SOME RESIDENT WHERE MANY MIGRATORY SONGBIRDS SUCH AS SCARLET MAMMALS SUCH AS WHITETAILED TANAGERS WARBLERS THRUSHES mY DEER WHICH ARE ALREADY EXPERI À>}iÌ>ÌÊ>`Ê CATCHERS AND VIREOS BREED 4HIS GAP ENCING RECORD HIGH POPULATIONS IS ACTUALLY WIDER THAN THE PORTION Ì iÊ`ÃÀÕ«ÌÊV>ÕÃi`Ê IN THE REGION AND ARE SEVERELY OF THE 'ULF OF -EXICO THAT MANY OF ALTERING FOREST GROWTH WITH THEIR LÞÊV>ÌiÊV >}iÊÜÊ THESE TROPICAL MIGRANTS MUST CROSS BROWSING 2EDUCED WINTER MOR 4HE NETWORKS OF WOODED STREAMS VÀi>ÃiÊÌ iÊ««ÀÌÕ TALITY DURING MILDER WINTERS MIGHT WOODLOTS AND EVEN URBAN FORESTS EXACERBATE THIS DAMAGE TO FORESTS ÌiÃÊvÀÊiÝÌVÊëiViÃÊ THAT DOT THE AGRICULTURAL PORTIONS OF -OOSE WHICH ARE ALREADY NEAR THIS GAP ARE CRITICAL STOPOVER AND ÌÊÛ>`iÊvÀiÃÌÃ]ÊvÕÀÌ iÀÊ THEIR SOUTHERN GEOGRAPHIC LIMIT REFUELING SITES FOR THE MIGRANTS IN THE REGION COULD BE NEGATIVELY ÃÌÀiÃÃ}Ê>ÌÛiÊëiVið #LIMATEDRIVEN SHIFTS IN THE TIMING IMPACTED BOTH BY WARMING AND OF TREE LEAFOUT SEED PRODUCTION BY THE INCREASING DENSITY OF DEER $EER CARRY THREE AND INSECT EMERGENCE HOWEVER MAY THROW THESE PARASITESBRAINWORM LIVER mUKE AND WINTER TICK WOODED REMNANTS OUT OF SYNC WITH THE BIRDS ARRIVAL THAT SEVERELY STRESS MOOSE #URRENTLY FOR INSTANCE MIGRATING SONGBIRDS 2EDUCED WINTER MORTALITY OF OMNIVOROUS MAM GATHER IN OAK TREES IN LARGE NUMBERS DURING SPRING MALS SUCH AS RACCOONS POSSUMS AND SKUNKS COULD MIGRATION TO CONSUME CATERPILLARS THAT ATTACK THE OAKS INCREASE THEIR OVERALL ABUNDANCE POTENTIALLY INCREAS DURING LEAFOUT A SITUATION MUTUALLY BENElCIAL TO THE ING PREDATION ON GROUNDNESTING SONGBIRDS AND TREES AND THE BIRDS "UT LEAFOUT OF TREES AND HATCH OTHER VULNERABLE PREY &IGURE ING OF CATERPILLAR EGGS IS CLOSELY TIED TO TEMPERATURE 4HE BENElTS OF WARMING FOR SOME RESIDENT MAM AND IS EXPECTED TO OCCUR 1,ÊÓ MALS AND BIRDS COULD BE COUNTERED BY POTENTIAL CHANGES EARLIER AS THE CLIMATE 6À}>Ê*ÃÃÕ½ÃÊ ,>}iÊÝ«>`}Ê ÀÌ IN THE DYNAMICS OF WILDLIFE DISEASES OR INCREASED WIN WARMS "ECAUSE MANY TER SURVIVAL OF PATHOGENS AND INSECT VECTORS 3UCH BIRDS MIGRATE IN RESPONSE EFFECTS WOULD BE MOST PRONOUNCED IN NORTHERN SPECIES TO DAY LENGTH RATHER THAT HAVE NOT BEEN EXPOSED TO OR EVOLVED DEFENSES THAN TEMPERATURE SOME AGAINST DISEASES FROM WARMER LATITUDES SONGBIRDS MAY ARRIVE #LIMATE CHANGE WILL ALSO INTERACT WITH FOREST FROM THE TROPICS WELL FRAGMENTATION PARTICULARLY IN HEAVILY AGRICULTURAL AFTER THE SPRING mUSH AREAS TO CREATE GREATER STRESS ON MANY BREEDING BIRDS OF INSECTS THAT ACCOM AND SOME REPTILES AND AMPHIBIANS 4HE IMPACT WILL PANIES LEAFOUT 4HE BE MOST SEVERE ON RELATIVELY IMMOBILE SPECIES RESTRICT SAME PHENOMENON MAY ING THEIR ABILITY TO MOVE NORTHWARD TO COLONIZE NEWLY APPLY TO THE mUSH OF -iiÊ«>}iÊ{n SUITABLE PATCHES OR ESCAPE NEWLY INHOSPITABLE CLIMATES SPRING INSECTS COMING vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi /N THE OTHER HAND SOME PREDATORS THAT ALREADY THRIVE OUT OF WETLANDS THAT ARE IN FRAGMENTED HABITATS WILL BENElT FROM WARMING VITAL TO MANY MIGRATORY SONGBIRDS 5NLIKE MIGRANTS 2AT SNAKES FOR EXAMPLE ARE MORE ACTIVE IN WARMER HOWEVER SOME YEARROUND RESIDENT BIRDS MAY BENElT TEMPERATURES IN FRAGMENTED HABITATS WHERE THEY ARE FROM WARMING A PHENOMENON THAT COULD FURTHER EXPOSED DIRECTLY TO SUNLIGHT ON THE FOREST EDGE STRESS MIGRATORY BIRDS SEE BOX P 3OME OF THESE PREDATORS WILL ALSO MOVE NORTH 0OPULAR GAMEBIRDS SUCH AS RUFFED GROUSE WHICH # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA INCREASING THE STRESSES ON NESTING BIRDS 3NAKES ARE DOMINANT NEST PREDATORS SOUTH OF THE #ORN "ELT BUT ARE ACTUALLY AN ENDANGERED SPECIES IN #ANADA WHERE THEY DEPEND HEAVILY UPON EDGE HABITATS &RAGMENTATION AND THE DISRUPTION CAUSED BY CLIMATE CHANGE WILL ALSO INCREASE THE OPPORTUNITIES FOR NON NATIVE SPECIES TO INVADE FORESTS PUTTING FURTHER PRES SURES ON NATIVE SPECIES }ÀVÕÌÕÀ>Ê>`ÃV>«ià 4 HE SIX 'REAT ,AKES STATES CONTAIN MILLION ACRES OF FARMLAND AND SEND MORE THAN BILLION 53 IN PRODUCTS TO MARKET !GRICUL TURAL PRODUCTION FROM MILLION ACRES OF FARMLAND IN /NTARIO IS VALUED AT BILLION #DN )N GENERAL LIVESTOCK IS MORE IMPORTANT IN THE NORTHERN AREAS -INNESOTA 7ISCONSIN WESTERN /NTARIO WHILE ROW CROPS DOMINATE THE SOUTHERN AREAS !LL OF THE 'REAT ,AKES STATES RANK IN THE TOP FOR THE VALUE OF DAIRY PRODUCTS AND CROPS SOLD NATIONALLY &IGURE 4HE REGION ALSO RANKS HIGH IN PRODUCTION OF HORTICULTURAL CROPS AND FRESH MARKET PRODUCTS FROM VEGETABLES TO FRUIT #ROP PRODUCTION IN THE REGION IS PRIMARILY RAINFED AND WEATHER IS THE MOST IMPORTANT UNCONTROLLED FACTOR INmUENCING CROP PRODUCTION 0RODUCTION CAN BE HARMED BY HEAT STRESS PESTS OZONE EXTREME WEATHER EVENTS SUCH AS RAINS THAT DELAY PLANTING OR HARVEST AND BELOWNORMAL PRECIPITATION ESPECIALLY DURING CRITICAL STAGES OF PLANT GROWTH SEE &IGURE P (ISTORICAL INmUENCES OF WEATHER ON YIELDS ARE DIFlCULT TO SEPARATE FROM THE INmUENCES OF TECHNOLOGICAL AND CULTURAL IMPROVEMENTS WHICH HAVE DRAMATICALLY IN CREASED YIELDS OVER THE PAST CENTURY BUT HAVE ALSO LED TO A TRANSFORMATION AND IN SOME CASES IMPOVERISH MENT OF THE 'REAT ,AKES REGIONAL LANDSCAPE >ÌiÊ«>VÌÃÊÊ À«Ã -OST PREDICTIONS FROM LARGESCALE SIMULATIONS SUGGEST THAT WHILE CLIMATE CHANGE IS LIKELY TO SHIFT CROP PRODUC TION PATTERNS THE REGIONS AGRICULTURAL CAPACITY IS UN LIKELY TO BE SERIOUSLY DISRUPTED OVER THE NEXT CENTURY )NDEED YIELD INCREASES OF TO PERCENT FOR MANY CROPS HAVE BEEN PROJECTED BASED ON EARLIER CLIMATE MODELS PROJECTING LESS WARMING ALTHOUGH THESE STUDIES CONCLUDED THAT TROPICAL OR WARMSEASON CROPS SUCH AS CORN MAY INCREASE LESS THAN SOYBEANS AND WHEAT !NOTHER RECENT ANALYSIS SUGGESTS THAT SOYBEAN BIOMASS COULD INCREASE BY PERCENT AND SOYBEAN YIELD BY PERCENT 3UCH PREDICTIONS REMAIN HIGHLY UNCER TAIN HOWEVER BECAUSE THE STRENGTH AND EVEN DIRECTION OF CROP RESPONSES CAN SHIFT WITH DIFFERENT CLIMATE CHANGE SCENARIOS 5NLESS TEMPERATURES ACTUALLY WARM BEYOND CROP GROWTH THRESHOLDS FACTORS OTHER THAN CLIMATE CHANGE WILL 1,ÊÎä HAVE AS GREAT OR GREATER Ýi`Ê«>VÌÃÊvÀÊ}ÀVÕÌÕÀi INFLUENCE ON TRENDS IN AGRICULTURE 4HESE FACTORS INCLUDE REGIONAL POPU LATION GROWTH ACCESS TO RESOURCES INCLUDING EMERG ING TECHNOLOGY AND MAR KET mUCTUATIONS 0RODUCERS MAY TAKE NO COMFORT IN PREDICTIONS FOR hAVERAGEv RESPONSES OF -iiÊ«>}iÊ{ CROP YIELDS TO VARIOUS vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi CLIMATE CHANGE FACTORS !VERAGES MASK SITETOSITE AND INCREASING YEARTOYEAR VARIABILITY IN YIELD WHICH AT THE FARM LEVEL TRANSLATES TO HIGHER RISK /NE STUDY OF IMPACTS OF CLIMATE VARI ABILITY ON FARMLEVEL RISK OF CROP FAILURE IN )LLINOIS AND 7ISCONSIN FOUND NOT SURPRISINGLY THAT RISK EXPOSURE WAS GREATER FOR SMALLER FARMS AND VARIED REGIONALLY AND AMONG CROPS 3UCH IMPACTS ON VARIABILITY AND RISK ARE LIKELY TO REINFORCE THE TREND TOWARD INCREAS ING FARM SIZE AND INDUSTRIALIZATION OF AGRICULTURE IN THE REGION -ODELS RUN AT SMALLER SCALES CONSISTENTLY SHOW THAT THE EFFECTS OF CHANGING CLIMATE WILL VARY ACROSS THE 'REAT ,AKES REGION /PTIMAL WEATHER CONDITIONS WILL SHIFT NORTHWARD AND EASTWARD TYPICALLY BRINGING THE GREATEST BENElTS TO -ICHIGAN -INNESOTA 7ISCON SIN AND EASTERN /NTARIO 3HIFTS IN THE DISTRIBUTION OF AGRICULTURE MAY BE CONSTRAINED IN NORTHERN AREAS BY THIN AND ACIDIC SOILS SEE &IGURE P )F MORE INTENSIVE PRODUCTION MOVES UPWARD FROM THE SOUTH ERN EDGE OF THE 'REAT ,AKES REGION ONTO SHALLOWER # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 4E R R E S T R I A L % C O S Y S T E M S COARSER TEXTURED SOILS EARLIER PLANTING DATES COULD INCREASE SOYBEAN YIELD IN THE NORTHERN AREAS UP TO PERCENT ABOVE CURRENT LEVELS IN THE CENTRAL CHEMICALS AND NUTRIENTS AND NORTHERN PORTIONS OF THE REGION )N THE SOUTHERN USED TO INCREASE SOIL FER AREAS COMPARATIVELY SMALL YIELD INCREASES TO TILITY MAY INCREASINGLY PERCENT OR SMALL DECREASES n TO n PERCENT RUN OFF INTO AQUATIC WERE PREDICTED 7HEAT YIELDS MAY ALSO INCREASE SYSTEMS !GRICULTURE IS APPROXIMATELY PERCENT AS A RESULT OF #/ FERTILI CURRENTLY A CHIEF SOURCE ZATION HOWEVER INCREASES RESULTING FROM EARLIER PLANT FOR CHEMICAL CONTAMINA ING DATES MIGHT BE LIMITED BECAUSE THEY OVERLAP THE TION OF GROUND AND SUR GROWING SEASON OF A PREVIOUS CROP FACE WATERS BUT THERE #/ FERTILIZATION MAY ALSO INmUENCE CROP YIELD -iiÊ«>}iÊ{ HAS BEEN LITTLE INVESTIGA IN INDIRECT WAYS )NITIAL RESULTS FROM A LARGESCALE EX vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi TION OF HOW REDISTRIBU PERIMENT THAT BEGAN IN #HAMPAIGN )LLINOIS IN TION OF AGRICULTURE IN SHOWED AS EXPECTED THAT ELEVATED #/ ENHANCED A CHANGING CLIMATE MAY INTERACT WITH THIS PROBLEM SOYBEAN YIELDS 4HE RESULTS ALSO INDICATED THAT ELEV /NE RECENT STUDY PROJECTED INCREASES IN PRODUC ATED #/ INCREASED THE WATER USE EFlCIENCY OF THE TION THANKS TO A LONGER GROWING SEASON AND WARMER SOYBEAN PLANTS A RESPONSE THAT HAS THE POTENTIAL TO TEMPERATURES BUT THAT STUDY RELIED ON A MODEL THAT REDUCE CROP WATER REQUIREMENTS AND REDUCE THE mUX PREDICTS PRECIPITATION TRENDS THAT ARE MUCH MORE FAVOR OF WATER INTO THE ATMOSPHERE ABLE FOR CROP PRODUCTION THAN THIS REPORT ASSUMES /ZONE CONCENTRATIONS CAN COUNTER POSITIVE TRENDS 9IELD TRENDS ARE LIKELY TO FALL SHORT OF THOSE PREDICTIONS IF IN CROP YIELDS JUST AS IN FOREST PRODUCTIVITY )N ADDI SUMMER RAINFALL DECREASES AS SUGGESTED BY THE CLIMATE TION TO URBAN SOURCES OF OZONE IN THE REGION AGRICUL SCENARIOS USED IN THIS REPORT SEE &IGURES AND TURAL APPLICATION OF FERTILIZERS CAN CAUSE LOCAL PEAKS IN P 4HESE SCENARIOS PROJECT WETTER PERIODS OCCUR OZONE LEVELS AND WARMER TEMPERATURES CAN ALSO INCREASE RING DURING TIMES THAT COULD DELAY HARVEST OR PLANTING OZONE FORMATION !LREADY REGIONAL OZONE CONCENTRA AND DRY SPELLS DURING TIMES WHEN CROPS DEMAND WATER TIONS FREQUENTLY REACH LEVELS THAT DAMAGE CROPS !S MODELS IMPROVE AND INCLUDE FACTORS SUCH AS EXTREME AND OZONE EXPOSURE IS CREDITED WITH CAUSING ALONE WEATHER EVENTS OR THE INmUENCE OF PESTS THEY ARE LIKELY OR IN COMBINATION WITH OTHER POLLUTANTS ABOUT TO PRODUCE LESS FAVORABLE OUTCOMES FOR AGRICULTURE PERCENT OF THE AIR POLLUTIONBASED CROP LOSSES /ZONE THAN HAVE BEEN PREDICTED DAMAGE IS EXPECTED TO TO DATE CAUSE LOCALIZED AREAS OF vÌiÀÊv>VÌÀ}ÊÊiÝÌÀiiÊÜi>Ì iÀÊ 4HE COMPLEXITY OF LOSSES IN SOYBEAN YIELDS AGRICULTURAL RESPONSES TO OF TO PERCENT IN iÛiÌÃÊÀÊÌ iÊvÕiViÊvÊ«iÃÌÃ]ÊÌ iÊ CLIMATE CHANGE IS HIGH THE -ISSISSIPPI AND /HIO «VÌÕÀiÊvÀÊ>}ÀVÕÌÕÀiÊÃÊiÃÃÊv>ÛÀ>LiÊ LIGHTED BY AN INTEGRATED VALLEYS 3IMILAR LOSSES ASSESSMENT THAT FOCUSED ARE PROJECTED FOR HORTI Ì >Ê«ÀiÛÕÃÊ«Ài`VÌÃÊÃÕ}}iÃÌi`° ON lVE UPPER -IDWEST CULTURAL CROPS WHICH STATES )LLINOIS )NDIANA ARE AT LEAST AS SENSITIVE -ICHIGAN /HIO AND 7ISCONSIN 4RENDS IN SOUTH TO OZONE DAMAGE AS SOYBEANS ERN AREAS OF /NTARIO WOULD BE EXPECTED TO RESEMBLE THOSE PROJECTED FOR -ICHIGAN 4HE ASSESSMENT PREDICT «>VÌÃÊÊ}ÀVÕÌÕÀ>Ê*iÃÌà ED MEAN INCREASES IN CORN YIELD OF PERCENT BUT THE 7ARMING TEMPERATURES MAY INmUENCE PEST AND RANGE OF BOTH INCREASES IN SOME NORTHERN AREAS DISEASE INCIDENCE IN SEVERAL WAYS &IRST WARMER AND TO PERCENT AND DECREASES IN SOUTHERN AREAS TO SHORTER WINTERS WILL ALLOW MORE SOUTHERLY PESTS SUCH n PERCENT WAS LARGE 4HE LARGEST CORNYIELD DECREASES AS CORN EARWORMS AND FALL ARMYWORMS TO EXPAND WERE PROJECTED FOR WESTERN )LLINOIS )N ADDITION THEIR RANGE NORTHWARD )NDEED SUCH A SHIFT ALREADY THE ASSESSMENT PREDICTED THAT #/ FERTILIZATION AND APPEARS TO BE HAPPENING WITH BEAN LEAF BEETLES WHICH 1,ÊΣ >ÌiÊ >}iÊ>`Ê}ÀVÕÌÕÀ>Ê*iÃÌà # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA PHYSIOLOGY OR FACILITY REQUIREMENTS $IRECT IMPACTS INCLUDE WARMER SUMMER TEMPERATURES THAT SUPPRESS APPETITE AND DECREASE WEIGHT GAIN IN ANIMALS &OR EXAMPLE A & # INCREASE IN TEMPERATURE IS PROJECT ED TO REDUCE ANIMAL PRODUCTIVITY BY PERCENT FOR BEEF AND DAIRY OPERATIONS IN THE SOUTHERN PARTS OF THE 5NITED 3TATES ALTHOUGH OTHER STUDIES PREDICT ONLY PERCENT LOSSES (IGHER TEMPERATURES ARE LIKELY TO REDUCE STOCKING RATES ON PASTURES AND CAN REDUCE MILK QUALITY BY REDUCING FORAGE QUALITY AND STRESSING ANIMALS !NY EXTREME WEATHER EVENTS SUCH AS HEAT WAVES DROUGHTS AND BLIZZARDS HAVE SEVERE EFFECTS ON LIVESTOCK HEALTH ALTHOUGH INTENSIVELY MANAGED LIVESTOCK OPERATIONS ARE BETTER ABLE TO BUFFER THE EFFECTS OF EXTREME EVENTS .EGATIVE IMPACTS ON 1 , Ê Î Î >ÌiÊ >}iÊ«>VÌÃÊ FORAGE AND GRASSLAND ÊÌ iÊ/LiÀÊ`ÕÃÌÀÞ PRODUCTIVITY AND FORAGE QUALITY CAN RESULT FROM SUMMER DROUGHT STRESS OR EXTREME WINTER WEATHER /NE STUDY PREDICTS THAT WARMER FALL TEMPERATURES WILL REDUCE FALL HARDENING OF FORAGE CROPS RENDERING THEM LESS HARDY DURING THE WINTER !DDITION ALLY THERE WILL BE LESS PRO -iiÊ«>}iÊ{ vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi TECTION BY SNOW COVER VVÊ ÃiµÕiViÃÊvÊ >ÌiÊ >`ÊV}V>Ê >}iÃÊÊ/iÀÀiÃÌÀ>Ê-ÞÃÌià ÀiÃÌÃÊ>`Ê7`vi OMMERCIAL FORESTRY IS A SUBSTANTIAL INDUSTRY IN NORTHERN PARTS OF THE REGION AND SIGNIl CANT FOREST PRODUCTS INDUSTRIES EXIST IN /N TARIO AND ALL 'REAT ,AKES STATES EXCEPT )LLINOIS &IGURE #LIMATE WARMING WILL DRIVE CHANGES IN FOREST EXTENT AND IN THE TYPES OF TREES FOUND IN VARIOUS PARTS OF THE REGION $URING THE TRANSITION HOWEVER WHILE TREES ILLSUITED TO NEW CLIMATE CONDITIONS PERSIST AND BETTERSUITED SPECIES ARE TAKING HOLD FOREST PRODUC TIVITY AND FOREST INDUSTRIES MAY SUFFER #HANGES IN THE TYPES OF TREES IN THE FOREST MAY ALSO BE JARRING TO MANY RESIDENTS SENSE OF PLACE 3HIFTS FROM BOREAL lR TO HARDWOOD FORESTS IN THE NORTHERN 'REAT ,AKES REGION COULD OCCUR IN THE LIFETIME OF CURRENT RESIDENTS FUNDAMENTALLY CHANGING THE CHAR ACTER OF THESE LOCATIONS 7HILE A hSENSE OF PLACEv IS FELT STRONGLY BY MANY PEOPLE IT IS HARD TO ASSIGN IT A DOLLAR VALUE EQUIVALENT TO DOLLAR VALUES FOR CHANGES IN HARVESTABLE TIMBER #HANGES IN FOREST COMPOSITION AND EXTENT WILL ALSO AFFECT WILDLIFE AND THE RECREATIONAL INDUSTRY THAT HAS GROWN UP AROUND HARVESTING OR WATCHING WILDLIFE !PPROXIMATELY MILLION ADULTS IN THE 'REAT ,AKES STATES PARTICIPATE IN BIRD WATCHING OR OTHER WILDLIFE VIEWING AND ANOTHER MILLION HUNT $ECLINES IN BIRD SPECIES WOULD HAVE DIRECT ECONOMIC CONSEQUENCES # IN TERMS OF HUNTING OR BIRD WATCHING AS WELL AS IN DIRECT CONSEQUENCES THROUGH LOSS OF THE BIRDS SERVICES IN CONTROLLING INSECTS AND OTHER PESTS 4HE LOSS OF GOOSE HUNTING FROM SOUTHERN )LLINOIS WHERE MORE THAN A MILLION GEESE ONCE WINTERED HAS SERIOUSLY AFFECTED THE ECONOMY OF ONE OF THE POOREST REGIONS OF THAT STATE }ÀVÕÌÕÀi 7HETHER CLIMATE CHANGE WILL BE ECONOMICALLY ADVANTAGEOUS OR HARMFUL FOR 'REAT ,AKES FARMERS REMAINS UNCERTAIN (OTTER DRIER SUMMER CONDITIONS WITH MORE FREQUENT DROUGHTS AS PREDICTED IN THIS REPORT COULD DISRUPT PRODUCTION ALTHOUGH INCREASED #/ FERTILIZATION COULD BOOST YIELDS OF SOME CROPS 4HE FATE OF AGRICULTURAL PRODUCTION WILL ALSO DEPEND UPON HOW CLIMATE CHANGE AFFECTS THE VARIABILITY AND PREDICTABILITY OF WEATHER PATTERNS %XTREME EVENTS SUCH AS SEVERE STORMS LATE SPRING OR EARLY FALL FROSTS AND DROUGHT ALL DEPRESS PRODUCTIVITY !PART FROM EXTREME EVENTS CROP FARMERS CAN ADAPT TO MODERATE CHANGES IN TEMPERATURE OR PRECI PITATION IF SUCH CHANGES CAN BE PREDICTED +NOWING THAT CONDITIONS WILL BE WARMER AND DRIER OR WARMER AND WETTER WILL ALLOW FARMERS TO PLANT CROP VARIETIES BETTER SUITED TO SUCH CONDITIONS )F THERE IS GREATER UNCERTAINTY HOWEVER FARMERS WILL NOT BE ABLE TO # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA 4E R R E S T R I A L % C O S Y S T E M S CHOOSE THE RIGHT VARIETIES FOR CONDITIONS THAT ACTUALLY OCCUR LEADING TO A MUCH GREATER RISK OF LOSS 4HUS THE IMPACTS OF CLIMATE CHANGE ON ANNUAL CROPS IN THE 'REAT ,AKES REGION APPEAR TO DEPEND MORE ON PREDIC TABILITY AND VARIABILITY OF WEATHER PATTERNS THAN THE CHANGE IN OVERALL AVER 1,ÊÎ{ AGES 'REATER CLIMATE «>VÌÃÊÊ-ÕiÀÊ,iVÀi>Ì VARIABILITY IS MORE PROB LEMATIC FOR PERENNIAL CROPS SUCH AS FRUIT TREES AND VINEYARDS WHERE ADJUSTMENTS CANNOT BE MADE AS FREQUENTLY AND LONGTERM INVESTMENTS ARE AT RISK #LIMATE CHANGES MAY ALSO AFFECT PROD -iiÊ«>}iÊxä UCTION COSTS )F DRIER vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi SUMMER CONDITIONS AND INCREASED DROUGHT PREVAIL INVESTMENTS IN IRRIGATION MAY BECOME NECESSARY 3UCH A SHIFT WOULD IMPOSE COSTS DIRECTLY ON FARMERS AND INCREASE TENSIONS OVER WATER ALLOCATIONS 7ITHOUT IRRIGATION HOWEVER AGRI CULTURAL PRODUCTIVITY CAN DROP SHARPLY DURING DROUGHT &OR EXAMPLE A DROUGHT REDUCED 53 CORN PRODUCTION BY PERCENT )NCREASED SOIL EROSION AND RUNOFF OF AGRICULTURAL WASTES ARE LIKELY IF THE FREQUENCY OF mOODING INCREASES 'REATER EROSION WOULD INCREASE OFFSITE COSTS OF SEDI MENTS WHICH ARE ALREADY ESTIMATED AT MILLION 53 FOR THE LAKE STATES OF -ICHIGAN -INNESOTA AND 7ISCONSIN AND MILLION 53 FOR THE #ORN "ELT STATES OF )LLINOIS )NDIANA )OWA -ISSOURI AND /HIO 7HATEVER THE OVERALL OUTCOME CERTAIN GROUPS MAY GAIN AT THE EXPENSE OF OTHERS &OR EXAMPLE IF CLIMATE CHANGE TENDS TO INCREASE PRODUCTION RESULTING PRICE DECLINES MAY HELP CONSUMERS BUT HURT PRODU CERS 2EGIONAL PRODUCERS WILL DO BETTER IF CLIMATE CHANGE LOWERS PRODUCTIVITY ELSEWHERE RESULTING IN LOWER SUPPLY AND HIGHER PRICES BUT DOES LITTLE TO CHANGE THEIR OWN PRODUCTIVITY )N AN ERA OF EXPANDING GLOBAL TRADE HOWEVER PRICES TO FARMERS AND COSTS TO CONSUMERS IN THE 'REAT ,AKES REGION MAY BE INmU ENCED MORE BY HOW DROUGHT OR RAIN IS PLAYING OUT IN CROP lELDS HALF A WORLD AWAY THAN BY HARVESTS AT HOME ,iVÀi>ÌÊ>`Ê/ÕÀà 4RAVEL AND TOURISM BROUGHT IN BILLION 53 IN REVENUE IN THE 'REAT ,AKES STATES IN AND BILLION #DN IN /NTARIO IN 4HE MOST CERTAIN IMPACTS OF CLIMATE CHANGE WILL BE ON WINTER SPORTS ACTIVITIES 7ARM WINTER TEMPERATURES AND LITTLE SNOW MEAN RED INK FOR SKI AREAS OR AT LEAST INCREASED COSTS FOR SNOWMAKING #OMMUNITIES AND BUSINESSES DEPEN DENT ON REVENUES FROM CROSSCOUNTRY OR DOWNHILL SKIING SNOWMOBILING OR ESPECIALLY ICE lSHING COULD BE HARD HIT 3OME OF THESE COMMUNITIES AND BUSI NESSES HOWEVER WILL MAKE UP THE LOSS BY EXPANDING WARM WEATHER TOURISM AND RECREATION &IGURE # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA #(!04%2 &IVE -EETING THE #HALLENGES OF #LIMATE #HANGE 4 HIS REPORT HAS HIGHLIGHTED A VARIETY OF CHALLENGES THE 'REAT ,AKES REGION WILL FACE AS CLIMATE CHANGE MAGNIlES THE PRESSURES IMPOSED BY A GROWING HUMAN POPULATION ON THE REGIONS ENVIRONMENT AND NATURAL RESOURCES -ANY OF THE IMPACTS EXPLORED HERE ARE NOT INEVITABLE 4HE NEGATIVE CONSEQUENCES OF CHANGE CAN IN SOME CASES BE MINIMIZED OR AVOIDED 4HIS CHAPTER EXAMINES ACTIONS THAT PEOPLE AND POLICYMAKERS CAN TAKE NOW TO REDUCE THE VULNERABILITY OF ECOSYSTEMS AND VITAL ECOLOGICAL SERVICES AND TO SAFEGUARD THE ECONOMY AND WELLBEING OF THE HUMAN POPULATION OF THE REGION 4HREE OVERLAPPING APPROACHES ARE NEEDED TO MEET THE CHALLENGES POSED BY A CHANGING CLIMATE 4HE lRST IS TO REDUCE THE REGIONS CONTRIBUTION TO THE GLOBAL PROBLEM OF HEATTRAPPING GREENHOUSE GAS EMISSIONS 3OME WARMING IS ALREADY INEVITABLE BECAUSE HISTORICAL EMISSIONS OF #/ WILL CONTINUE TO HAVE A WARMING EFFECT FOR DECADES NEVERTHELESS MANY OF THE MOST EXTREME OUTCOMES FOR THE REGION CAN BE AVOIDED IF THE PACE AND EVENTUAL SEVERITY OF CLIMATE CHANGE ARE DAMPED -ANY SCIENTISTS AGREE THAT ULTIMATELY WORLD WIDE EMISSIONS OF HEATTRAPPING GASES NEED TO BE RE DUCED SIGNIlCANTLY IN ORDER TO AVOID DANGEROUS CHANGES IN THE CLIMATE SYSTEM 4HE SOONER THESE REDUCTIONS ARE BEGUN THE LOWER THE COST OF MAKING NECESSARY CHANGES AND DEALING WITH POTENTIALLY DISRUPTIVE ECONOMIC AND SOCIAL IMPACTS 3ECOND MINIMIZING HUMAN PRESSURES ON THE GLOBAL AND LOCAL ENVIRONMENT NOW WILL LESSEN THE SEVERITY OF FUTURE IMPACTS AND REDUCE THE VULNERABILITY OF ECO SYSTEMS TO FURTHER STRESSES FROM CLIMATE &INALLY ANTI CIPATING AND PLANNING FOR THE IMPACTS OF CHANGE THROUGH BOTH SHORTTERM ADJUSTMENTS AND LONGTERM ADAPTA TIONS WILL HELP TO REDUCE FUTURE DAMAGE 4HE COST OF THESE ADJUSTMENTS AND ADAPTATIONS SERVE AS AN ADDI TIONAL INCENTIVE TO SLOW CLIMATE CHANGE BY REDUCING THE EMISSIONS OF HEATTRAPPING GASES AS SOON AS POSSIBLE !LTHOUGH THERE IS UNCERTAINTY IN PREDICTIONS OF SPECIlC CLIMATE CHANGE IMPACTS ON THE REGION WE HAVE MUCH GREATER CONlDENCE IN THE GENERAL PREDIC TIONS FOR CHANGE SEE BOX P %VEN WHERE UNCER TAINTY REMAINS TAKING ACTIONS NOW TO REDUCE EMIS SIONS AND MINIMIZE THREATS TO ECOSYSTEMS IS THE PRUDENT AND RESPONSIBLE COURSE 7AITING TO BEGIN REDUCING EMISSIONS OR TO PLAN FOR MANAGING THE EFFECTS OF CLIMATE CHANGE ONLY INCREASES THE EVENTUAL EXPENSE AND URGENCY AND THE POSSIBILITY OF IRREVERSIBLE LOSSES &URTHERMORE MANY ACTIONS THAT CAN BE TAKEN NOW PROVIDE IMMEDIATE COLLATERAL BENElTS SUCH AS COST SAVINGS CLEANER AIR AND WATER OR IMPROVED QUALITY OF LIFE IN OUR COMMUNITIES # / . & 2/ . 4 ) . 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MORE CONTROVERSIAL ISSUE CONCERNING FUTURE WATER SUPPLIES INVOLVES SCHEMES TO DIVERT WATER TO USERS OUT SIDE THE BASIN 3UCH DIVERSIONS WOULD HAVE SIGNIlCANT ECOLOGICAL AND SOCIAL IMPLICATIONS FOR THE ENTIRE 'REAT ,AKES BASIN AND POTENTIALLY CREATE LEGAL POLICY AND PROCEDURAL CONmICTS WITHIN THE REGION 1ÀL>Ê>`Ê>`Ê1ÃiÊ*>}Ê 5RBAN AND RURAL LAND USE PLANNING CAN REDUCE SPRAWL WHICH IN TURN REDUCES GREENHOUSE GAS EMISSIONS FROM COMMUTER TRAFlC 2EDUCING SPRAWL HAS ADDED BENElTS OF PREVENTING HABITAT DESTRUCTION AND FRAGMENTATION REDUCING OR AT LEAST CONTAINING THE AREA OF IMPERVIOUS SURFACES THAT CONTRIBUTE TO mOODING REDUCING MUNIC IPAL SPENDING ON SERVICES AND DECREASING THE LOSS OF VALUABLE FARMLAND &IGURE )N 'RAND 2APIDS -ICHIGAN WHICH IS QUICKLY BECOMING THE POSTERCHILD OF THE NATIONS GROWING ANTISPRAWL MOVEMENT A CIVIC CAMPAIGN LED TO COMPREHENSIVE LANDUSE POLICY RE FORMS INCLUDING PRESERVATION OF CONNECTED OPEN LANDS AND NATURAL AREAS ESTABLISHMENT OF COMPACT BUSINESS CENTERS SERVED BY MASS TRANSIT AND ESTABLISHMENT OF BOUNDARIES ON EXTENDING WATER AND SEWER SERVICES >LÌ>ÌÊ*ÀÌiVÌÊ>`Ê,iÃÌÀ>Ì 2EHABILITATION OF WOODED RIPARIAN BUFFER STRIPS RES TORATION OF mOODPLAIN FORESTS WETLAND PRESERVATION AND RESTORATION AND REDUCTION OF THE EXTENT OF IM PERVIOUS SURFACES ARE STRATEGIES THAT HELP TO MAIN /ÊÊÊÝ>«iÃÊvÊ`>«ÌÛiÊi>ÃÕÀiÃÊvÀÊÌ}>Ì}Ê«>VÌÃÊ ÊvÊ >ÌiÊ >}iÊÊà iÀiÃÊ `>«Ì>ÌÊ -ÌÀ>Ìi}Þ ÃiÉ >}i\ V>Ì 1Ãi ,i`ÕViÊÃÃiÃ\ *ÀiÛiÌÊivviVÌ `vÞÊivviVÌ -«iVwÊVÊ"«Ì Ì>Ìà VÕÀ>}iÊwÊà iÀÃÊÌÊÛiÊwÊà }Ê }ÀÕ`ÃÊ>ÃÊV>ÌÃÊvÊ«ÀiviÀÀi`ÊwÊÃ Ê >LÌ>ÌÊV >}i ÃÌÊÃÌVÃÊvÊ`iÃÀ>LiÊwÊà ÊëiViÃÊ>ÀiÊ i>ÛÞÊiÝ«Ìi`Ê>Ài>`Þ Ý«ÌÊ«ÀiÛÕÃÞÊÕÕÃi`ÊÀÊÕ`iÀÕÃi`Ê ÀiÃÕÀViÃÊ V>Ê>µÕ>ÌVÊiVÃÞÃÌiÃÊÜÊLiViÊ }iiÀ>ÞÊÛiÀiÝ«Ìi`Ê>ÃÊÌ iÊvVÕÃÊvÊ wÊà iÀÃÊiÝÌi`ÃÊÌÊ>ÊiÛiÃÊvÊÌ iÊv`ÊÜiLÊ ÌÊ«ÃÃLi ÀÌwÊV>ÞÊ>VViiÀ>ÌiÊ>ÌÕÀ>ÊÀ>ÌiÃÊvÊ À>}iÊiÝÌiÃÊvÀÊÜ>ÀÜ>ÌiÀÊëiVià >ÀiiÃÃÊ>VÌÃÊÜÊiÝ>ViÀL>ÌiÊ«ÀLià ,i`ÕViÊ«>VÌÃÊvÀÊÌ iÀÊ>}iÌÃÊ vÊÃÌÀiÃÃÆÊ«>ÀÌVÕ>ÀÞÊÀiiÛ>ÌÊvÀÊ wÊà iÀiÃÊV>Ìi`ÊÊ>Ài>ÃÊvÊ } Ê Õ>Ê ««Õ>ÌÊ`iÃÌÞ ,iÃÃÌ>ViÊÌÊÌÊ`iÃÌÀÕVÌÛiÊiÛÀiÌ>Ê «>VÌÃÊvÊ`ÕÃÌÀÞÊ>`ÊÌ iÀÊ Õ>Ê >VÌÛÌià ,iÛiÊ«ÌiÌ>ÊL>ÀÀiÀÃÊÌÊ}À>ÌÊ >`ÊÀ>}iÊiÝÌiÃÊ VVi«ÌÊÃÃiÃ\ - >ÀiÊÃà Êi>ÀÊÃà «iÃ>ÌÉÃÕÀ>ViÊ«À}À>ÃÊ vÀÊwÊà iÀà ÊÌ }ÊÌÊÃ>ÛiÊëiViÃÊÀÊÃÌVà -ÕV Ê>VÌÃÊ«ÀÛ`iÊÞÊà ÀÌ ÌiÀÊÌ}>Ì]ÊvÊÌ iÊ«ÀiV«Ì>Ì}Ê iÛÀiÌ>ÊV >}iÃÊ>ÀiÊ«iÀ>iÌ # / . & 2/ . 4 ) . 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ROBUST STRAT EGY IN THE FACE OF UNCERTAINTY OR EVEN UNPREDICTABIL ITY IS ONE THAT WILL BE mEXIBLE ENOUGH TO FARE WELL UNDER A WIDE RANGE OF 1,ÊÎ POSSIBLE OUTCOMES 4HE V}V>ÊÌÃÊÌÊ`>«Ì>ÌÊ Ê}ÀVÕÌÕÀi SECTIONS BELOW DESCRIBE SOME hNO REGRETSv AC TIONS THAT MAY BE TAKEN TO MANAGE THE IMPACTS OF CLIMATE CHANGE ON THE 'REAT ,AKES ECONO MY PEOPLES AND EN VIRONMENT à iÀià 4HE HISTORIES OF ABOR -iiÊ«>}iÊxÓ IGINAL COMMERCIAL AND vÀÊvÕÃâiÊVÀÊ>}iÊvÊÌ ÃÊwÊ}ÊÕÀi SPORT lSHERIES PROVIDE MANY EXAMPLES OF THE ADAPTABILITY OF lSHERS 7HEN TRADITIONALLY EXPLOITED STOCKS FAIL EFFORT IS QUICKLY REDIRECTED AND lSHING METHODS ARE ADJUSTED TO OTHER STOCKS AND SPECIES ,IKEWISE AS REGIONAL WATERS WARM lSHERIES MAY BE ABLE TO ADAPT TO A NEW MIX OF lSH SPECIES 4HIS DOES NOT MEAN HOWEVER THAT INDIVIDUAL lSHERS OR SPECIlC lSHING COMMUNITIES WILL NECESSARILY AVOID SERIOUS NEGATIVE EFFECTS IN PART BECAUSE HABITS AND CULTURAL PREFERENCES ARE TYPICALLY SLOW TO CHANGE 4ABLE P %FFECTIVE ADAPTATION WILL LIKELY INVOLVE REALLOCATION OF HARVEST FROM ADVERSELY AFFECTED POPULATIONS SUCH AS LAKE TROUT IN SOUTHERN INLAND LAKES TO POPULATIONS THAT ARE POSITIVELY AFFECTED SUCH AS WALLEYE IN NORTHERN WATERS AND SMALLMOUTH BASS THROUGHOUT THE BASIN (OWEVER THE lSH COMMUNITY MAY FACE A PROLONGED PERIOD OF RESTRUCTURING WHILE PRODUCTIVITY AND WATER TEMPERATURES ARE IN TRANSITION 4HIS TRANSITIONAL STAGE MAY CREATE GREAT UNCERTAINTY IN DETERMINING SUSTAINABLE HARVESTS OF ANY lSH SPECIES !LSO BOTH lSHERMEN AND CONSUMERS HAVE PREFERENCES FOR PARTICULAR SPECIES THAT MAY BE DIFlCULT TO CHANGE AND MAY PROLONG EXPLOITA TION OF POPULATIONS THAT SHOULD BE PROTECTED /VERALL ROBUST lSHERIES MANAGEMENT SHOULD BE GUIDED BY SOME BASIC PRINCIPLES INCLUDING s -AINTAINING EXPLOITATION RATES AT LEVELS THAT INCLUDE A SAFETY MARGIN BASED ON HISTORICAL UNCERTAINTIES IN FISH STOCKS s 2EDUCING THE NEGATIVE IMPACTS OF OTHER HUMAN STRESSORS SUCH AS ACIDIFICATION AND HABITAT DESTRUCTION s )NITIATING CONCERTED EFFORTS TO REDUCE OVERINVEST MENT IN A FISHERY THAT CAN EXPLOIT CERTAIN SPECIES AT UNSUSTAINABLE RATES s %NSURING THAT NO PRACTICE APPLIED FOR A SHORT TIME COULD PRODUCE EXTREME OUTCOMES µÕ>ÌVÊVÃÞÃÌiÃ]Ê,iÃÕÀViÃ]Ê>`Ê7`vi 4O HELP SUSTAIN AQUATIC RESOURCES AND ECOSYSTEMS EFFORTS SHOULD FOCUS ON PROTECTING RIPARIAN ZONES OF RIVERS EXISTING WETLANDS AND HEADWATER STREAMS GROUNDWATER SYSTEMS AND LAKES 0ROTECTING AND REVEGETATING RIPARIAN ZONES FOR EXAMPLE CAN YIELD A LARGE RETURN ON INVESTMENT IN TERMS OF REDUCING DAM AGES AND ECONOMIC LOSSES FROM mOODING AND IMPROV ING WATER QUALITY .ATIVE SPECIES CHOSEN FOR SUCH PROJ ECTS SHOULD BE EVALUATED IN TERMS OF THEIR SUITABILITY FOR A WARMER CLIMATE AND THEIR ABILITY TO WITHSTAND FREQUENT mOODS AND DROUGHTS 4O BOOST THE CHANCES # / . & 2/ . 4 ) . 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REPORT OF THE .ATIONAL 7ATER !SSESS MENT 'ROUP FOR THE 53'#20 /AKLAND #ALIF 0ACIlC )NSTITUTE FOR 3TUDIES IN $EVELOPMENT %NVIRONMENT AND 3ECURITY ,EWANDOWSKI * AND $ 3CHIMMELPFENNING %CONOMIC IMPLICATIONS OF CLIMATE CHANGE FOR 53 AGRI CULTURE !SSESSING RECENT EVIDENCE ,AND %CONOMICS n $ALE 6( ET AL #LIMATE CHANGE AND FOREST DISTURBANCE "IO3CIENCE n )RLAND ,# ET AL !SSESSING SOCIOECONOMIC IMPACTS OF CLIMATE CHANGE ON 53 FORESTS WOOD PRODUCT MARKETS AND FOREST RECREATION "IO3CIENCE n # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA #ONTRIBUTING !UTHORS iÀ}iÊ} THE LEAD AUTHOR OF THIS REPORT IS A PROFESSOR OF BIOLOGY IN THE $EPARTMENT OF %COLOGY AND %VOLUTIONARY "IOLOGY AT THE 5NIVERSITY OF -ICHIGAN (IS AREAS OF SPECIAL IZATION INCLUDE LIMNOLOGY THE STUDY OF LAKES AND STREAMS CLIMATE CHANGE BIOGEOCHEMISTRY AND ECOSYSTEM SCIENCE (E HAS RESEARCH PROGRAMS THAT STUDY THE FUNCTIONING OF AQUATIC ECOSYSTEMS IN THE !RCTIC THE TROPICS AND THE TEMPERATE ZONE $R +LING RECEIVED A .ATIONAL !CADEMY OF 3CIENCES 2ESEARCH )NVESTIGATOR AWARD AND A 5NITED .ATIONS 3ASAKAWA #ERTIFI CATE OF -ERIT AND HE IS A .ATIONAL 3CIENCE &OUNDATION 0RESI DENTIAL &ACULTY &ELLOW AND A FELLOW OF THE !!!3 (E HAS PARTICIPATED IN OVER INTERNATIONAL PANELS REVIEW BOARDS AND CONFERENCES HELD BY .3& .2# AND 5.%3#/ MANY OF WHICH INVOLVED ISSUES OF GLOBAL CHANGE $R +LING RECEIVED HIS 0H$ IN FROM $UKE 5NIVERSITY >Ì >ÀiÊ>Þ i IS AN INDEPENDENT RESEARCH CONSULTANT SPECIALIZING IN THE SCIENCEPOLICY INTERFACE (ER AREAS OF EX PERTISE INCLUDE THE IMPACT OF HUMAN ACTIVITIES ON CLIMATE GREENHOUSE GAS EMISSIONS AND CONTROL POLICIES AND NUMERICAL MODELING OF THE EARTHATMOSPHERE SYSTEM -S (AYHOE RECEIVED HER -3 IN !TMOSPHERIC 3CIENCES FROM THE 5NIVER SITY OF )LLINOIS AT 5RBANA#HAMPAIGN (ER CLIENTS AND COLLAB ORATORS SPAN A WIDE RANGE OF GOVERNMENT AND PRIVATE AGEN CIES ON BOTH SIDES OF THE BORDER INCLUDING %NVIRONMENT #ANADA THE %NVIRONMENTAL 0ROTECTION !GENCY THE .ATIONAL 2OUND 4ABLE ON %NERGY THE %NVIRONMENT THE /NTARIO -INISTRY OF %NERGY THE %NVIRONMENT AND THE $EPART MENT OF %NERGY 2ECENTLY SHE HAS BEEN FUNDED BY THE )LLINOIS)NDIANA 3EA 'RANT THROUGH THE 5NIVERSITY OF )LLINOIS TO EVALUATE PROJECTIONS OF CLIMATE CHANGE FOR THE 'REAT ,AKES AREA 3HE PROVIDED THE ANALYSES OF HISTORICAL CLIMATE DATA AND FUTURE MODEL PROJECTIONS USED AS THE BASIS OF IMPACT ASSESSMENTS THROUGHOUT THE REPORT ÕV`>Ê Ã IS THE !SSOCIATE $IRECTOR OF THE #ENTER FOR 7ATER AND THE %NVIRONMENT .ATURAL 2ESOURCES 2ESEARCH )NSTITUTE 5NIVERSITY OF -INNESOTA $ULUTH (ER RESEARCH FOCUSES ON QUANTIFYING THE EFFECTS OF LAND USE AND GEOLOGY ON HABITAT AND BIOTA IN WETLANDS AND STREAMS !NOTHER RESEARCH EMPHASIS INCLUDES THE DEVELOPMENT OF INDICATORS OF STREAM AND WETLAND ECOSYSTEM CONDITIONS USING AMPHIBIANS INVERTEBRATES AND FISH AS FOCAL SPECIES !S A LANDSCAPE AND AQUATIC ECOLOGIST SHE HAS BEEN INVOLVED IN RESEARCH AND DIS CUSSIONS ABOUT THE CAUSAL FACTORS OF FROG MALFORMATIONS OVER THE PAST FIVE YEARS 4HE MAJORITY OF HER WORK HAS TAKEN PLACE IN THE -IDWESTERN 5NITED 3TATES AND IN THE 'REAT ,AKES "ASIN WITH A PARTICULAR EMPHASIS ON AGRICULTURAL LANDSCAPES )N THIS REPORT SHE CONTRIBUTED TO SECTIONS ABOUT LAND USE PATTERNS AND CONFOUNDING EFFECTS OF HUMAN DISTURBANCES ON ECOSYS TEMS AFFECTED BY CLIMATE CHANGE AS WELL AS SECTIONS ON THE ECOLOGICAL IMPACTS ON RIVERS WETLANDS AND AMPHIBIANS $R *OHNSON RECEIVED HER 0H$ FROM -ICHIGAN 3TATE 5NIVERSITY AND HAS WORKED IN HER CURRENT POSITION AT THE .ATURAL 2ESOURCES 2ESEARCH )NSTITUTE SINCE ,V >À`Ê`ÀÌ IS 0ROFESSOR OF %COLOGY IN THE $EPART MENT OF %NTOMOLOGY AT THE 5NIVERSITY OF 7ISCONSIN-ADISON (IS RESEARCH INTERESTS INCLUDE THE IMPACTS OF GLOBAL ENVIRON MENTAL CHANGE EG ELEVATED CARBON DIOXIDE TROPOSPHERIC OZONE AND 56 RADIATION ON PLANTS AND PLANTFEEDING INSECTS $R ,INDROTH RECEIVED HIS 0H$ IN ECOLOGY FROM THE 5NIVER SITY OF )LLINOIS5RBANA FOLLOWED BY AN .3& 0OSTDOCTORAL &ELLOWSHIP AT THE 5NIVERSITY OF 7ISCONSIN )N HE RECEIVED A &ULBRIGHT 3ENIOR 2ESEARCH 3CHOLAR AWARD TO STUDY THE IMPACTS OF ENHANCED 56 RADIATION IN .EW :EALAND $R ,INDROTH HAS SERVED ON THE EDITORIAL BOARDS OF SEVERAL JOUR NALS IN ECOLOGY AND ON GRANT REVIEW PANELS FOR THE .ATIONAL 3CIENCE &OUNDATION AND 53 $EPARTMENT OF !GRICULTURE )N THIS REPORT HE CONTRIBUTED TO SECTIONS DEALING WITH INSECT RESPONSES TO CLIMATE CHANGE Ê°Ê>}Õà IS AN %MERITUS 0ROFESSOR OF :OOLOGY AND PAST $IRECTOR OF THE #ENTER FOR ,IMNOLOGY AT THE 5NIVERSITY OF 7ISCONSIN-ADISON (IS RESEARCH INTERESTS ARE IN LONG TERM REGIONAL ECOLOGY FISH AND FISHERIES ECOLOGY AND THE EFFECTS OF CLIMATE CHANGE AND VARIABILITY ON INLAND WATERS BIODIVERSITY AND INVASIONS (E PLAYED A LEAD ROLE IN THE LAKES AND STREAMS PORTIONS OF THE AND !SSESSMENTS BY )NTERGOVERNMENTAL 0ANEL ON #LIMATE #HANGE (E HAS SERVED ON THE 3CIENCE !DVISORY "OARDS OF THE )NTERNATIONAL *OINT #OMMISSION ON 7ATER 1UALITY AND THE 'REAT ,AKES &ISHERIES #OMMISSION (E SERVED ON THE /CEAN 3TUDIES "OARD OF THE .ATIONAL 2ESEARCH #OUNCIL AND HAS CHAIRED SEVERAL #OMMIT TEES FOR .2# $R -AGNUSON HAS AUTHORED MORE THAN PUBLICATIONS AND FIVE BOOKS AND WAS 0RINCIPAL )NVESTIGATOR OF THE .ORTH 4EMPERATE ,AKES ,ONG4ERM %COLOGICAL 2ESEARCH 3ITE (E EARNED HIS 0H$ FROM 5NIVERSITY OF "RIT ISH #OLUMBIA #ANADA IN ZOOLOGY WITH A MINOR IN OCEANO GRAPHY )N THIS REPORT HE CONTRIBUTED TO SECTIONS ON LAKES ICE WETLANDS FISHERIES AND SOLUTION STRATEGIES # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . ' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA -ÕÃ>iÊÃiÀ IS STAFF SCIENTIST FOR CLIMATE CHANGE AT THE 5NION OF #ONCERNED 3CIENTISTS (ER CURRENT WORK FOCUSES ON PROVIDING SOUND SCIENTIFIC INFORMATION TO SUPPORT POLICY MAKING ON CLIMATE CHANGE (ER RESEARCH INTERESTS INCLUDE CLIMATE CHANGE IMPACTS ON COASTAL AREAS ENVIRONMENTAL HAZ ARDS THE HUMAN DIMENSIONS OF GLOBAL CHANGE AND THE INTER ACTION BETWEEN SCIENCE AND POLICY $R -OSER RECEIVED HER 0H$ IN 'EOGRAPHY FROM #LARK 5NIVERSITY 7ORCESTER -ASS AND COMPLETED A TWOYEAR POSTDOCTORAL RESEARCH FELLOWSHIP AT (ARVARDS +ENNEDY 3CHOOL OF 'OVERNMENT BEFORE JOINING 5#3 /VER THE LAST YEARS SHE HAS PARTICIPATED IN REVIEWS OF %0!S 'LOBAL #HANGE 0ROGRAMS THE 53 'LOBAL #HANGE 2ESEARCH 0ROGRAM AND ITS SUCCESSOR THE #LIMATE #HANGE 3CIENCE 0ROGRAM AS WELL AS OF VARIOUS CHAPTERS OF )0## AND 53 .ATIONAL !SSESSMENT REPORTS )N THIS REPORT SHE CONTRI BUTED TO SECTIONS DEALING WITH CLIMATE CHANGE IMPACTS ON URBAN AREAS HUMAN HEALTH AND SOLUTIONS STRATEGIES -Ìi« iÊ*>ÃÞ HOLDS THE &ESLER,AMPERT #HAIR IN %COLOGICAL%NVIRONMENTAL %CONOMICS AT THE 5NIVERSITY OF -INNESOTA (E IS A FACULTY MEMBER OF THE $EPARTMENT OF !PPLIED %CONOMICS AND OF THE $EPARTMENT OF %COLOGY %VO LUTION AND "EHAVIOR AND IS ALSO CODIRECTOR OF 'RADUATE 3TUDIES FOR THE #ONSERVATION "IOLOGY 0ROGRAM (E RECEIVED HIS 0H$ IN ECONOMICS FROM THE 5NIVERSITY OF -ICHIGAN IN (E IS CURRENTLY SERVING AS A MEMBER OF THE %NVIRON MENTAL %CONOMICS !DVISORY #OMMITTEE OF 53 %0!S 3CIENCE !DVISORY "OARD AS A MEMBER ON A .ATIONAL 2ESEARCH #OUNCIL #OMMITTEE ON !SSESSING AND 6ALUING 3ERVICES OF !QUATIC AND 2ELATED 4ERRESTRIAL %COSYSTEMS AND AS #O#HAIR FOR #ORE 0ROJECT $EVELOPING THE 3CIENCE OF #ONSERVATION AND 3US TAINABLE 5SE OF "IODIVERSITY FOR $)6%23)4!3 (IS RESEARCH INTERESTS INCLUDE BIODIVERSITY CONSERVATION AND ENDANGERED SPECIES POLICY INTEGRATING ECOLOGICAL AND ECONOMIC ANALYSIS GAME THEORY APPLICATIONS TO NATURAL RESOURCE USE COMMON PROPERTY RESOURCES AND ENVIRONMENTAL REGULATION (E RECENTLY EDITED A BOOK ENTITLED 4HE %CONOMICS OF "IODIVERSITY #ONSERVA TION )N THIS REPORT HE CONTRIBUTED TO SECTIONS ON THE ECONO MIC IMPACTS OF CLIMATE CHANGE AND CLIMATE CHANGE SOLUTIONS -VÌÌÊ,Là IS A PROFESSOR IN THE $EPARTMENT OF !NI MAL "IOLOGY AT THE 5NIVERSITY OF )LLINOIS (IS RESEARCH INTERESTS INCLUDE THE EFFECTS OF FOREST FRAGMENTATION ON MIGRATORY BIRDS ESPECIALLY DURING THE BREEDING SEASON -OST OF HIS RECENT WORK HAS BEEN IN THE -IDWESTERN 5NITED 3TATES BUT HE HAS ALSO WORKED EXTENSIVELY IN THE .EOTROPICS AND IN .ORTH !MERICAN GRASSLANDS AND SCRUBLANDS (IS STUDENTS ALSO WORK ON EFFECTS OF GLOBAL CLIMATE CHANGE ON THE TIMING OF MIGRATION AND ON THE EFFECTS OF HYDROLOGY ON BIRDS OF FLOODPLAIN FORESTS $R 2OBINSON HAS ALSO BEEN INVOLVED IN DEVELOPING MANAGEMENT PLANS FOR GRASSLAND AND FOREST RESERVES $R 2OBINSON RECEIVED HIS 0H$ FROM 0RINCETON 5NIVERSITY !S OF -AY HE WILL BE MOVING TO THE &LORIDA -USEUM OF .ATURAL (ISTORY 5NIVERSITY OF &LORIDA WHERE HE WILL BE THE +ATHERINE /RDWAY #HAIR OF %COSYSTEM #ONSERVATION )N THIS REPORT HE CONTRIBUTED TO SECTIONS ON THE EFFECTS OF GLOBAL CLIMATE CHANGE ON WILDLIFE À>Ê- ÕÌiÀ IS A RESEARCH SCIENTIST WITH THE /NTARIO -INIS TRY OF .ATURAL 2ESOURCES AND ADJUNCT PROFESSOR IN THE $EPART MENT OF :OOLOGY 5NIVERSITY OF 4ORONTO (IS RESEARCH HAS FOCUSED ON THE POPULATION DYNAMICS OF FRESHWATER FISH AND PARTICULARLY ON THE ROLE OF WEATHER IN GENERATING SHORTTERM VARIATION IN ABUNDANCE AND THE ROLE OF CLIMATE IN SHAPING BOUNDARIES OF SPECIES DISTRIBUTIONS (E HAS WORKED ON POPULA TIONS OF SMALLMOUTH BASS WALLEYE AND LAKE TROUT IN THE 'REAT ,AKES AND IN THE SMALLER LAKES OF !LGONQUIN 0ARK (E HAS AUTHORED OVER PAPERS IN THE PEER REVIEWED SCIENTIFIC LITERATURE AND IS A MEMBER OF THE "OARD OF 4ECHNICAL %XPERTS OF THE 'REAT ,AKES &ISHERIES #OMMISSION $R 3HUTER WORKED ON THE LIMNOLOGY AND FISHERIES SECTIONS OF THIS REPORT V iiÊ7>`iÀ IS AN ASSOCIATE PROFESSOR IN THE 5NIVERSITY OF )LLINOIS $EPARTMENT OF .ATURAL 2ESOURCES AND %NVIRON MENTAL 3CIENCES WHERE SHE TEACHES ABOUT SOIL ECOLOGY COM POSITION AND PROCESSES AND ADVISES BOTH GRADUATE AND UNDER GRADUATE STUDENTS 3HE HAS SERVED AS THE #HAIR OF THE .ORTH #ENTRAL 2EGION #OMMITTEE ON 3OIL /RGANIC -ATTER AND "IOCHEMISTRY ON 53$!.2) 2EVIEW 0ANELS FOR 3OIL "IOLOGY AND "IOCHEMISTRY AND -ANAGED %COSYSTEMS AND HAS PARTICI PATED AS AN EXPERT ON TEAMS EVALUATING LONGTERM AGRICUL TURAL STUDIES 3HE IS AN !SSOCIATE %DITOR FOR THE 3OIL 3CIENCE 3OCIETY OF !MERICA 333! *OURNAL AND NOW SERVES ON THE COMMITTEE FOR THE 3PECIAL 0UBLICATION 3OIL #ARBON -ANAGE MENT 'UIDE AS WELL AS THE !D (OC #OMMITTEE ON 'LOBAL %NHANCEMENT OF 3OIL /RGANIC -ATTER $R 7ANDER RECEIVED HER 0H$ IN IN !GRONOMY3OIL 3CIENCE FROM THE /HIO 3TATE 5NIVERSITY )N THIS REPORT SHE CONTRIBUTED SECTIONS ON AGRICULTURAL RESPONSE TO CLIMATE CHANGE AND POTENTIAL MITIGATION AND ADAPTATION STRATEGIES >ÀÊ7à IS CURRENTLY $IRECTOR OF THE 'LOBAL (EALTH 0ROGRAM AND !SSOCIATE 0ROFESSOR OF %PIDEMIOLOGY AT THE 5NIVERSITY OF -ICHIGAN WHERE HIS RESEARCH AND TEACHING COVER THE BROAD AREA OF ECOLOGY AND EPIDEMIOLOGY OF INFECTIOUS DISEASES !FTER EARNING HIS DOCTORAL DEGREE FROM (ARVARD 5NI VERSITY IN HE WORKED AT THE 0ASTEUR )NSTITUTE IN $AKAR 3ENEGAL n WAS ON THE FACULTY AT THE 9ALE 5NIVERSITY 3CHOOL OF -EDICINE n AND THEN JOINED THE 5NIVERSITY OF -ICHIGAN $R 7ILSONS RESEARCH ADDRESSES THE ENVIRON # / . & 2/ . 4 ) . 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' % ) . 4 ( % ' 2 % !4 , ! + % 3 2 % ' ) / . 5NION OF #ONCERNED 3CIENTISTS s 4HE %COLOGICAL 3OCIETY OF !MERICA MENTAL DETERMINANTS OF ZOONOTIC AND ARTHROPODBORNE DISEASES THE EVOLUTION OF VECTORHOSTPARASITE SYSTEMS AND THE ANALYSIS OF TRANSMISSION DYNAMICS (E IS AN AUTHOR OF MORE THAN JOURNAL ARTICLES BOOK CHAPTERS AND RESEARCH REPORTS AND HAS SERVED ON NUMEROUS GOVERNMENTAL ADVISORY GROUPS CONCERNED WITH ENVIRONMENTAL CHANGE AND INFECTIOUS DISEASE EPIDEMIOLOGY (E RECENTLY SERVED AS A MEMBER OF THE .2# PANEL ON #LIMATE %COSYSTEMS )NFECTIOUS $ISEASES AND (UMAN (EALTH AND THE )/- PANEL ON %MERGING -ICRO BIAL 4HREATS IN THE ST #ENTURY (E CONTRIBUTED TO THE HEALTH IMPACTS SECTIONS AND SOLUTIONS IN THIS REPORT >`Ê7ÕiLLià IS (EAD OF THE $EPARTMENT OF !TMO SPHERIC 3CIENCES AT THE 5NIVERSITY OF )LLINOIS AND 0ROFESSOR IN THAT DEPARTMENT AS WELL AS IN THE $EPARTMENT OF %LECTRICAL AND #OMPUTER %NGINEERING (IS RESEARCH HAS EMPHASIZED THE DEVELOPMENT AND USE OF MATHEMATICAL MODELS OF THE ATMOSPHERE TO STUDY THE CHEMICAL AND PHYSICAL PROCESSES THAT DETERMINE ITS STRUCTURE (E IS THE AUTHOR OF OVER SCIENTIFIC ARTICLES AND DIRECTS A NUMBER OF RESEARCH PROJECTS TO IMPROVE OUR UNDERSTANDING OF THE IMPACTS THAT HUMANMADE AND NATURAL TRACE GASES MAY BE HAVING ON THE %ARTHS CLIMATE ATMOSPHERIC CHEMISTRY AND OZONE (E DEVELOPED THE CON CEPT OF /ZONE $EPLETION 0OTENTIALS 0OTENTIALS± ±USED ± USED IN MOST POLICY MAKING TO PROTECT THE OZONE LAYER EG THE -ONTREAL 0ROTOCOL AND ITS AMENDMENTS±AND ±AND IS COAUTHOR OF AN ± ANALOGOUS CONCEPT 'LOBAL 7ARMING 0OTENTIALS CURRENTLY USED TO DESCRIBE GREENHOUSE GASES AND THEIR POTENTIAL EFFECTS ON CLIMATE $R 7UEBBLES HAS LED THE DEVELOPMENT OF SEVERAL NEW RESEARCH CENTERS AT THE 5NIVERSITY OF )LLINOIS INCLUDING A CENTER ON THE REGIONAL IMPACTS OF CLIMATE CHANGE ON THE -IDWEST (E IS A LEAD AUTHOR ON A NUMBER OF INTER NATIONAL ASSESSMENTS RELATED TO STRATOSPHERIC OZONE AND CLIMATE CHANGE $R 7UEBBLES LED THE ANALYSIS OF REGIONAL EFFECTS OF CLIMATE CHANGE FOR THIS REPORT $ONALD :AK IS A PROFESSOR IN THE 3CHOOL OF .ATURAL 2E SOURCES AND %NVIRONMENT AT THE 5NIVERSITY OF -ICHIGAN (IS RESEARCH FOCUSES ON THE FUNCTION OF SOIL MICROBIAL COM MUNITIES IN THE BIOGEOCHEMICAL CYCLING OF CARBON AND NITRO GEN IN TERRESTRIAL ECOSYSTEMS (E AND SEVERAL COLLEAGUES HAVE ESTABLISHED LARGESCALE FIELD EXPERIMENTS TO INVESTIGATE THE INFLUENCES OF RISING ATMOSPHERIC #/ AND / ON FORESTS IN THE UPPER 'REAT ,AKES 4HEY ALSO HAVE INITIATED LONG TERM EXPERIMENTS TO STUDY THE INFLUENCE OF ATMOSPHERIC NITROGEN DEPOSITION ON FOREST IN THE REGION $R :AK SERVES ON THE EDITORIAL BOARDS OF %COLOGY %COLOGICAL -ONOGRAPHS AND 3OIL 3CIENCE 3OCIETY OF !MERICA (E RECEIVED HIS 0H$ DEGREE FROM -ICHIGAN 3TATE 5NIVERSITY CONDUCTED POST DOCTORAL RESEARCH AT THE 5NIVERSITY OF -INNESOTA AND HAS BEEN A 0ROFESSOR AT THE 5NIVERSITY OF -ICHIGAN SINCE $R :AK CONTRIBUTED TO SECTIONS ON FOREST AND FORESTRY IMPACTS AS WELL AS IMPACTS ON OTHER TERRESTRIAL ECOSYSTEMS IN THIS REPORT 3TEERING #OMMITTEE ! NATIONAL STEERING COMMITTEE PROVIDED GUIDANCE AND OVERSIGHT TO ENSURE THE SCIENTIlC REVIEW AND INTEGRITY OF THE REPORT 4HE 3TEERING #OMMITTEE MEMBERS WERE À°ÊÕÃÊ°Ê*Ìi> #HAIR !PPALACHIAN ,ABORATORY 5NIVERSITY OF -ARYLAND #ENTER FOR %NVIRONMENTAL 3CIENCE &ROSTBURG -D À°Ê>ÀÞÊ>ÀLiÀ %COLOGICAL 3OCIETY OF !MERICA 7ASHINGTON $# À°Ê ÀÃÌ« iÀÊi` #ARNEGIE )NSTITUTION OF 7ASHINGTON $EPARTMENT OF 0LANT "IOLOGY 3TANFORD #ALIF À°Ê*iÌiÀÊ °ÊÀÕ vv 5NION OF #ONCERNED 3CIENTISTS #AMBRIDGE -ASS À°ÊivvÊi> #OLUMBIA 5NIVERSITY 'RADUATE 3CHOOL OF "USINESS .EW 9ORK .9 À°ÊiÀÀÞÊi -ARINE "IOLOGICAL ,ABORATORIES 7OODS (OLE -ASS À°ÊÕ`ÞÊiÞiÀ 5NIVERSITY OF 'EORGIA )NSTITUTE OF %COLOGY !THENS 'A À°Ê7>Ê-V iÃ}iÀ $UKE 5NIVERSITY .ICHOLAS 3CHOOL OF THE %NVIRONMENT $URHAM .# À°Ê-ÌiÛiÊ-V i`iÀ 3TANFORD 5NIVERSITY $EPARTMENT OF "IOLOGICAL 3CIENCES AND THE )NSTITUTE FOR )NTERNATIONAL 3TUDIES 3TANFORD #ALIF # / . & 2/ . 4 ) . ' # , ) - !4 % # ( ! . 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