/+(*08.4(&%+.80+.&0 +/8/0)(47/.+//+4*0&*+4/ .&*0/&**5&.+*)*0(+*0.+(/* */0 &/04.*/ ;(&/*((;5&; +((8.*.;&0%%&0%+4/;+%* .*';&((&)//)*;4(.++'/;+( &.)*;4/4)0%*&;%/'.&0.; >+3'8 *&5./&08+8+)&*$;*&5./&08+ .&9+*;1+*(*0.+.0)+/,%.& /.%;*&000/+./0.5&; D4 (+ 4*&*$=$7,0;;; %+0+/8*0%/&/*8.4(&+4,(&*$ • • • • A = photosynthetic CO2 assimilation GS =canopy stomatal conductance CA = ambient CO2 concentration CI = internal CO2 concentration KL = plant hydraulic conductance Ψ = water potential of soil (s) and leaf (L) SGE H SFG&'@/6H SFGΨDΨHG.8@/6H SFNCFGΨDΨHG+**0&'*.8H • S)&*G.+78(1+*G)7HK(0.+*0.*/,+.0GHH G.-%4.GNRQM0>H)+(H – 4*04)8&(-4*1!/*+,8/%&*$&),0 • 4/1040%8.4(&+*0.+(/+5.G04(0(>OMMPH – SIFNCGΨDΨHFNCGE HJF)&*G)7KH – – *'*+6*/&$*(+**1+*/ 8.4(&&)&01+*/0+*+,8 0.*/,&.1+*GH KL = hydraulic conductance GS =canopy stomatal conductance Ψ = water potential soil or leaf EL = transpiration per leaf (LAI) or canopy VPD = vapor pressure deficit EL ΨL EC=EL·LAI GS=EL / VPD Ψ Sap flux KL =EL / (ΨS -ΨL) ΨS GS=KL·1/VPD·(ΨS -ΨL) GS response to light and VPD Oren et al. 1999; Ewers et al. 2000; Ewers et al. 2005 6+,,.+%/0+(&*$,&* , Paint-byNumbers Spatial Gradient GS = canopy stomatal conductance D = vapor pressure deficit m = GS sensitivity to D /1*$,(*0%8.4(&0%+.8.+///,&/;(51+**)+.0(&08 Engelmann spruce/subalpine fir (~3,180 m) Sagebrush (~2,100 m) Lodgepole pine (~2,750 m) ,1(3.*/%*$6&0%),+.(.&5./ Increased driving force for EC in time changed EC spatial patterns as individual tree hydraulics become limiting EC = canopy transpiration D = vapor pressure deficit range = distance of spatial autocorrelation Adelman et al Tree Phys. 2008 Low elevation sagebrush has high transpiration and conductance per unit leaf due to access to light, but steep response to both atmospheric and soil water limitation Naithani et al In Review m = sensitivity of canopy conductance to VPD GSref = reference canopy stomatal conductance Across ~1000 m elevation gradient and species differences, plant limitations due to soil and atmospheric drought fit expectations from plant hydraulics; strong isohydric water potential regulation A = leaf CO2 assimilation PPFD = visible light photons Species differences in photosynthesis reflect leaf life span and climate expectations; little impact from drought so ecosystem C uptake can be predicted from gas exchange limits by plant hydraulics .+)$.*0./? +.0./?&*(//0%*8. John Frank John Frank (4/0&*4*$& &),00.*/,&.1+* -4&'(8 #.+*)+*0%;0.*/,&.1+* ,.0.&/.40+(//0%*%( 40+%8.4(&(&)&01+*/.+) 4*$(78()+(4/&+* m = sensitivity of canopy conductance to VPD GSref = reference canopy stomatal conductance Blue stain impacts on hydraulics fit expectation of simple plant hydraulic model, slope of m to Gsref between 0.5 and 0.6; Englemann spruce is nearly less sensitive, explained by spruce biology (McDowell et al 2002; Ewers et al 2005) A = leaf CO2 assimilation PPFD = visible light photons Blue stain/bark beetles do not impact leaf photosynthetic biochemistry; hydraulic limitation leads to decreased C uptake during mortality phase of bark beetle outbreak Bark Beetle Epidemic &)4(0 .41+*&* ;.&0; +((+6/8 +5.&*0 .+).'0( ,&)&&* OMMQ*OMMR E-transpiration, Ecrit-E rate at hydraulic failure from cavitation (Sperry et al 1998 model), NEE-net ecosystem exchange of CO2; simulations in TREES model (Mackay et al 2003, Ewers et al 2008, Mackay et al In press)--net result--plant hydraulic theory predicts bark beetle/ blue stain impacts on ecosystem carbon and water cycling +/8/0)&),(&1+*/ • (*0%8.4(&0%+.8,.&0/(.$/( /,&/*(51+*%*$/&*,(*060. 4//6((//)((/(/0*/,1( 5.&&(&08 • *.$8(&)&0+./0/6&0%.'0( ,&)&%5A&(((+$&(B('+/0.)"+6 &*./40+ • (&3(/*+6,'%*$ • (//(&*&*.+)(+6.0.*/,&.1+* +),*/08&*./5,+.1+* G.++'/0(0('0%&/)+.*&*$H +/8/0)&),(&1+*/ • *+,8+*40*(&*7,(&*/0 +/8/0)7%*$+O4.&*$.' 0()+.0(&08 G.*'/0(+/0.<0(+/0.0%&/ #.*++*H • )+(,///0/0+.'0( )+.0(&088&*(4&*$%8.4(&(&)&01+*/0+ ,.&05,+0.*/,&.1+***0 +/8/0)7%*$+O G'80(+/0.8/0.8#.*++*H