Global, National, and Regional Effects of Climate Change on Plants and Animals Dr. David Karowe Department of Biological Sciences Western Michigan University Overview of this evening’s talk 1. Observed changes since 1900 a. b. c. d. Temperature Moisture Phenology (seasonal timing) Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions What’s been happening to Earth’s temperature? Temperature Change (oC) Since 1900, Earth has warmed ~ 0.8o C 10 warmest years in history: 2010, 2005, 2007, 2009, 1998*, 2002, 2003, 2006, 2004, and 2008 http://data.giss.nasa.gov/gistemp/graphs/ Temperature difference relative to 1950-1980 http://data.giss.nasa.gov/gistemp/animations/ Can climate change be due to “natural variation”? Since 1900, energy increase from greenhouse gasses is about 20 times energy increase from the sun1 Solar Irradiance For the last 30 years, solar irradiance has been decreasing2 Since 1900, natural factors would have caused a slight cooling3 Since 1950, Ohio has warmed by ~0.8 oC http://data.giss.nasa.gov/gistemp/maps/ Last year, Ohio was ~0.75o C above the 1951-1980 mean http://data.giss.nasa.gov/gistemp/maps/ This summer, Ohio was much warmer than normal http://www.ncdc.noaa.gov/sotc/service/national/Statewidetrank/201106-201108.gif Overview of this evening’s talk 1. Observed changes since 1900 a. Temperature b. Moisture c. Phenology (seasonal timing) d. Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions Since 1900, no consistent trend in global precipitation4 But severe storms have become more common5 43% increase in Ohio since 1948 59% increase in Cleveland Severe storms cause flooding, erosion, disease This year, Ohio had its wettest April and 5th wettest February on record http://www.ncdc.noaa.gov/temp-and-precip/maps As a result, Ohio experienced flooding this spring Overview of this evening’s talk 1. Observed changes since 1900 a. Temperature b. Moisture c. Phenology (seasonal timing) d. Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions Many plant species now leaf out and flower significantly earlier6 - e.g. of 385 British species, 16% now flower significantly earlier than in 1954-1990 - only 3% flowered significantly later Earlier Later In Ohio, budburst for white oak is now 23 days earlier than around 1900 May 3 → April 10 (data provided by Kellen Callinger, OSU) In Trumbull County, wild pansy has been tracking climate change since 1900 (7 days earlier per 1o C warming) - but toothwort has not Viola rafinesquii Cardamine diphylla - overall, 34 of 56 species show significant flowering advancement (data provided by Kellen Callinger, OSU) Plant speices that have been tracking climate change have fared better than species that have not - in Thoreau Woods, major declines for species without phenological advancement over the last 150 years7 e.g. asters, anemones, ericales, violets, roses, lilies, dogwoods, orchids, and mints Days per decade In general, animals are speeding up more than plants8 Increased ecological asynchrony is likely to cause problems Butterflies: 3.7 days/decade Herbs, grasses, and shrubs: 1.1 days/decade Trees: 3.3 days/decade Overview of this evening’s talk 1. Observed changes since 1900 a. Temperature b. Moisture c. Phenology (seasonal timing) d. Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions Few changes in geographic ranges have been documented for plants, other than altitudinal shifts e.g. the hardwood-conifer transition zone on Vermont mountains moved upslope ~100 meters from 1962-20059 sugar maple, beech, and yellow birch have replaced red spruce, balsam fir, and paper birch More range changes have been documented for animals - many taxonomic groups are expanding polewards10 What does the future hold? Overview of this evening’s talk 1. Observed changes since 1900 a. Temperature b. Moisture c. Phenology (seasonal timing) d. Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions Earth is expected to warm by at least 2-4o C by 210011 “Business as usual” Alternate energy sources 4o 2o 0.6o Zero emissions CO2 has an atmospheric residence time of >100 years When Earth was 5o cooler, Michigan was covered with ice12 Temperature rise is likely to persist for >1,000 years after we stop emitting greenhouse gasses13 Predicted warming in Ohio of 3.5-4.0o C by 210014 What will happen to extreme temperature events? Globally, more and stronger heat waves15 Future summers are very likely to be hotter than any experienced thus far16 Ohio would experience many more days above 90o F17 Ohio would experience many more days above 90o F17 Ohio would experience many more days above 90o F17 Cleveland would experience ~60 days over 90o F18 - and about 21 days over 100o F And at least one heat wave per summer like the one that killed ~700 people in Chicago in 199518 Overview of this evening’s talk 1. Observed changes since 1900 a. Temperature b. Moisture c. Phenology (seasonal timing) d. Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions More severe rainstorms19 But also more and stronger droughts19 - global land area in extreme drought is predicted to increase from 1% to 30% 20 Summer rainfall predicted to decrease throughout U.S.17 Breadbasket could become largely unsuitable for agriculture By the end of the century, Ohio summers may feel like those of current-day Arkansas http://www.ucsusa.org/greatlakes/winmigrating/glwinmig_oh.html Overview of this evening’s talk 1. Observed changes since 1900 a. Temperature b. Moisture c. Phenology (seasonal timing) d. Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions What is the likely future fate of species? Climate Envelope Modeling is used to predict future changes in geographic range and population size 1. Determine the levels of important climate variables (usually temperature and precipitation) that occur within the species’ current geographic range 2. Use climate model(s) to predict where those levels will exist in the future (= future suitable habitat) 3. Make an assumption about dispersal (usually “full” or “none”) 4. Compare current and future ranges to infer population increase or decrease Woodland horsetail is predicted to decline due to decreased geographic range21 current future Wild peony is predicted to increase current future Fate of European cohosh is unclear, since it must migrate to reach its future habitat ? On average, forest herbs will have to move ~6 mi/year - but most show current rate of ~ 5 feet/year - and dispersal routes are limited by lack of European forests Required range shifts Forest cover ≥ 35% of these species face a moderate/high extinction risk21 Even if suitable future habitat exists, species may not be able to get there in time to avoid extinction ? Most studies predict many more losers than winners 5-25% extinction of Australian Banksia species22 Huge losses are predicted for 5,200 African plant species, even with full dispersal23 - 40% species extinction by 2085 - population decline for 80-97% of species In Ohio, sugar maple is predicted to almost disappear with climate change24 Future Current FutureHigh Low 10 of the 20 most abundant Ohio tree species are predicted to decline by at least 50% -100% White pine -100% Bigtooth aspen -91% Sugar maple -89% Black cherry -79% -78% White ash American beech Three of the 20 most abundant Ohio tree species are predicted to increase Black gum +14% Black oak +112% Post oak +150-fold Several rare tree species are predicted to increase dramatically in Ohio Winged elm +6-fold Sweetgum +43-fold Shortleaf pine +104-fold - and many southern species are predicted to arrive Ohio forests are predicted to change fairly dramatically25 Future Future Current High Low Major loss of Amazon rainforest with 2.5o rise (?)26 - lost carbon storage Animals are also likely to be affected by climate change African mammals are likely to be adversely affected Of 227 species, 20% are predicted to be extinct by 2080 even with full dispersal27 - 40% extinction with no dispersal Two areas of highest species loss Congo Basin Kalahari region Species lost European boreal bats are likely to be adversely affected28 - 100% of boreal and temperate species show range loss Adverse effects also for European Mediterranean bats - 71% of Mediterranean species show range loss Most Western Hemisphere amphibian species are predicted to be adversely affected by climate change29 of 413 species: ⅔ lose >50% of range ⅜ lose >90% of range area of greatest vulnerability Globally, lizard species are predicted to experience up to 20% extinction by 208030 - tropical species are more vulnerable Local Birds in high northern latitudes are particularly vulnerable to habitat loss due to climate change31 27 northern species lose, on average, 74-84% of suitable habitat by 2080 White-winged Crossbill Eurasian Dotterel Montane bird species are also highly vulnerable32 - globally, 18% of 1,009 species are predicted to lose at least half of their geographic range by 2100 32% 38% The U.S. Forest Service has made predictions about the fate of 129 Ohio bird species by 2100:33 Current Future A rea-weighted Incidence 300.0 250.0 200.0 150.0 100.0 50.0 0.0 1 6 11 16 21 26 31 36 41 46 51 56 61 66 71 76 81 86 91 96 101 106 111 116 121 126 131 136 Species 80 species (62%) are predicted to decrease 49 species (38%) are predicted to increase 36 Ohio bird species are predicted to decline by >90% -100% Savannah Sparrow -99% Bank Swallow -99% House Wren -98% Tree Swallow -99% -99% Veery Bobolink -98% Willow Flycatcher -96% Cedar Waxwing Another 19 species are predicted to decline by 50-90% -89% -88% song sparrow Yellow Warbler -74% Cerulean Warbler -82% -81% Blue-winged Warbler -69% Rose-breasted Grosbeak American Redstart -56% Ovenbird -53% American Goldfinch 32 species are predicted to increase by >50% +660-fold +113-fold +104-fold Chuck-will’s Widow* Black Vulture* Loggerhead Shrike* +5-fold Summer Tanager +103% Northern Bobwhite +77% Yellow-billed Cuckoo +7-fold Pine Warbler* +58% Carolina Wren 10 new species are predicted to occur in Ohio Brown-headed Nuthatch Mississippi Kite Little Blue Heron Snowy Egret Scissor-tailed Flycatcher Painted Bunting Cattle Egret Bachman’s Sparrow Globally, if we allow Earth to warm by 3o C, 20-50% of species may be committed to extinction26 Overview of this evening’s talk 1. Observed changes since 1900 a. Temperature b. Moisture c. Phenology (seasonal timing) d. Geographic ranges 2. Predicted future changes a. Temperature b. Moisture c. The fate of species 3. Solutions Are there any solutions? Yes! Unfortunately, energy conservation is not a solution - really just delays the inevitable 48 mpg Emissions reductions need to be rapid and large - 80% reduction by 2050 to avoid worst scenarios34 Urgent need for alternate energy sources solar wind A solar array 100 x 100 miles could provide all of US electricity needs today35 Wind power could supply 16 times current U.S. electricity demand36 Globally, can wind and solar supply enough energy?36,37 10,000 6,000 4,000 2,000 2100 8,000 Today Energy (EJ/yr) 12,000 0 Global Demand Wind Potential Solar Potential Sources of information cited in this talk 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. IPCC (Intergovernmental Panel on Climate Change). 2007. Fourth Assessment Report, Chapter 2, Changes in Atmospheric Constituents and Radiative Forcing, Section 2.9.2. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch2s2-9-2.html Lockwood, M. and C. Froehlich. 2008. Recent oppositely directed trends in solar climate forcings and the global mean surface air temperature. II. Different reconstructions of the total solar irradiance variation and dependence on response time scale. Proc. Roy. Soc. A 464: 1367-1385. IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 9, Understanding and Attributing Climate Change, Section 9.4.1.2. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch9s9-4-1-2.html IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 3, Observations: Atmospheric Surface and Climate Change, Section 3.2.2. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch3s3-2-2.html Madsen, T. and E. Figdor. 2007. When it rains, it pours: Global warming and the rising frequency of extreme precipitation in the United States. Environment Rhode Island Research and Policy Center. www.environmentrhodeisland.org. Root, T., J. Price, K. Hall, S. Schneider, C. Rosenzweig and J. Pounds. 2003. Fingerprints of global warming on wild animals and plants. Nature 421: 57-60. Willis, C., B. Ruhfel, R. Primack, A. Miller-Rushing, and C. Davis. 2008. Phylogenetic patterns of species loss in Thoreau’s woods are driven by climate change. Proc. Natl. Acad. Sci. 105: 17029-17033. Parmesan, C. 2007. Influences of species, latitudes and methodologies on estimates of phenological response to global warming. Global Change Biology 13: 1860-1872. Beckage, B., B. Osborne, D. Gavin, C. Pucko, T. Siccama, and T. Perkins. 2008. A rapid upward shift of a forest ecotone during 40 years of warming in the Green Mountains of Vermont. Proc. Natl. Acad. Sci. USA 105: 4197-4202. Hickling, R., D. Roy, J. Hill, R. Fox, and C. Thomas. 2006. The distributions of a wide range of taxonomic groups are expanding polewards. Global Change Biology 12: 450-455. IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 10, Global Climate Projections, Section 10.3. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch10s10-3.html Christopherson, R. 2000. Geosystems: An Introduction to Physical Geography (4th ed). Prentice-Hall, NY. Solomon, S., G.-K. Plattner, R. Knutti and P. Friedlingstein. 2009. Irreversible climate change due to carbon dioxide emissions. Proc. Natl. Acad. Sci. 106: 1704-1709. IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 11, Regional Climate Projections, Section 11.5.3. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch11s11-5-3-2.html IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 10, Global Climate Projections, Section 10.3.6.2. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch10s10-3-6-2.html Battisti, D. and R. Naylor. 2009. Historical warnings of future food insecurity with unprecedented seasonal heat. Science 323: 240-244. Sources of information cited in this talk (cont.) 17. 18. 19. 20. 21. 22. 23. 24. 25. 26. 27. 28. 29. 30. 31. 32. Karl, T., J. Melillo and T. Peterson (eds). 2009. Global Climate Change Impacts in the United States. National Climate Change chapter. http://downloads.globalchange.gov/usimpacts/pdfs/National.pdf. Union of Concerned Scientists. 2009. Confronting Climate Change in the U.S. Midwest – Ohio. http://www.ucsusa.org/assets/documents/global_warming/climate-change-ohio.pdf. IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 10, Global Climate Projections, Section 10.3.6.1. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch10s10-3-6-1.html. Burke, E.J., S.J. Brown, and N. Christidis. 2006. Modelling the recent evolution of global drought and projections for the twenty-first century with the Hadley Centre climate model. J. Hydrometeorol. 7: 1113-1125. Skov, F. and J.-C. Svenning. 2004. Potential impact of climatic change on the distribution of forest herbs in Europe. Ecography 27: 366-380. Fitzpatrick, M., A. Gove, N. Sanders and R. Dunn. 2008. Climate change, plant migration, and range collapse in a global biodiversity hotspot: the Banksia (Proteaceae) of Western Australia. Global Change Biology 14:1-16. McClean, C.J., J. Lovett, W. Kuper, L. Hannah, J. Sommer, W. Barthlott, M. Termansen,G. Smith, S. Tokumine, and J. Taplin. 2005. African plant diversity and climate change. Ann. Missouri Bot. Gard. 92:139-152. Prasad, A. M., L. R. Iverson., S. Matthews., M. Peters. 2007-ongoing. A Climate Change Atlas for 134 Forest Tree Species of the Eastern United States [database]. Northern Research Station, USDA Forest Service, Delaware, Ohio. http://www.nrs.fs.fed.us/atlas/tree/tree_atlas.html. Prasad, A. M., L. R. Iverson., S. Matthews., M. Peters. 2007-ongoing. http://www.nrs.fs.fed.us/atlas/tree/ft_summary.html. IPCC. 2007. Fourth Assessment Report, Working Group II, Chapter 4, Ecosystems, their properties, goods, and services, Section 4.4.11. http://www.ipcc.ch/publications_and_data/ar4/wg2/en/ch4s4-4-11.html. Thuiller, W., O. Broennimann, G. Hughes, J. Roberts, M. Alkemades, G. Midgley, and F. Corci. 2006. Vulnerability of African mammals to anthropogenic climate change under conservative land transformation assumptions. Global Climate Biology 12: 424-440. Rebelo, H., P. Tarroso and G. Jones. 2010. Predicted impact of climate change on European bats in relation to their biogeographic patterns. Global Change Biology 16: 561-576. Lawler, J., S. Shafer, B. Bancroft and A. Blaustein. 2009. Projected climate impacts for the amphibians of the western hemisphere. Conservation Biology 24: 38-50. Sinervo,B., F. Méndez-de-la-Cruz, D. Miles, et al. 2010. Erosion of lizard diversity by climate change and altered thermal niches. Science 328: 894-899. Virkkala R., R. K. Heikkinen, N. Leikola, and M. Luoto. 2008. Projected large-scale range reductions of northernboreal land bird species due to climate change. Biological Conservation 141:1343-1353. LaSorte, F. and W. Jetz. 2010. Projected range contractions of montane biodiversity under global warming. Proc. R. Soc. B 277: 3401-3410. Sources of information cited in this talk (cont.) 33. 34. 35. 36. 37. Matthews, S.N., L. R. Iverson, A.M. Prasad, A. M., and M.P. Peters. 2007-ongoing. A Climate Change Atlas for 147 Bird Species of the Eastern United States [database]. Northern Research Station, USDA Forest Service, Delaware, Ohio. http://www.nrs.fs.fed.us/atlas/bird. National Academy of Sciences of the United States. 2010. Climate Stabilization Targets: Emissions, Concentrations, and Impacts over Decades to Millenia. http://dels.nas.edu/resources/static-assets/materials-basedon-reports/reports-in-brief/Stabilization-Targets-Final.pdf America's Solar Energy Potential. http://www.americanenergyindependence.com/solarenergy.aspx. Lua, X., M. McElroy and J. Kiviluoma. 2009. Global potential for wind-generated electricity. Proc. Natl. Acad. Sci. 106: 10933-10938. IPCC. 2007. Fourth Assessment Report, Working Group III, Chapter 4, Energy Supply, Section 4.3. http://www.ipcc.ch/publications_and_data/ar4/wg3/en/ch4s4-3.html