environmental limits of the biological carbon pumping in the forests
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EnvironmentalEnvironmental limitslimits ofof thethebiologicalbiological carboncarbon pumpingpumping
in in thethe forestsforestseffecteffect ofof thethe solarsolar radiationradiation type type
–– dimmingdimming effecteffect
Michal V. Marek, Michal V. Marek, OtmarOtmar Urban,Urban,Dalibor Dalibor JanouJanoušš
Centre Centre forfor GlobalGlobalChangeChange ImpactImpact StudieStudie
Forest trees and the light
EffectsEffects ofof solarsolar radationradation energyenergy
Photo-energetic effect – photosynthesis, transpiration
Photo-cybernetic effect – induction vegetative/generative phase changes
Photo-destructive effect - inhibiton of photosynthesis, chlorophyll bleachning
Incident Incident solarsolar radationradation
Global solar radiation – whole radiation
Beam solar radiation – direct solar beams
Diffusive solar radiation – multidirectional illumination
DimmingDimming effecteffect
ObservedObserved reductionreduction of the solar radiation intenzity up to
0.51 ± 0.05 W m-2 per year, i.e. 2.7 % per decenium
TheThe causescauses ofof thethe „„globalglobal dimmingdimming““increase of the antropogenic pollutansincrease of the water vapour atmosphericvulcanic activity
enhancedenhanced diffusivediffusive solarsolar radiationradiation
Merkado L.M. et al.: Nature 458: 1014-1018, 2009.
El Chichón Pinatubo
net primary production (NPP) is enhanced in realtion to the diffusive conditions
Diffusive radiation was responsible for the increasedcarbon sink in the years period 1960 - 1999 up to 25%
DiffusiveDiffusive solarsolar radiationradiation enhancesenhances NPPNPP
0
400
800
1200
1600
0:00 6:00 12:00 18:00 0:00
Time, h
PPFD
, μm
ol m
-2 s
-1CloudySunny
ExampleExample ofof dailydaily coursecourse ofof PAR PAR underunder BEAM BEAM andand DIFUSSIVEDIFUSSIVE conditonsconditons
Merkado L.M. et al.: Nature 458:
1014-1018, 2009.
Urban O. et al.: GCB 46: 157-168, 2007.
Diffusive solar radiation enhanced GPP and NPP
-10
-5
0
5
10
15
20
25
30
0 500 1000 1500PPFD (μmol m-2 s-1)
NEE
(μm
ol m
-2 s
-1)
CloudySunny AMSunny PMFit
A
ComparisonComparison ofof thethe „„beambeam“ versus „“ versus „diffusivediffusive“ “ daysdays effectseffectson on carboncarbon uptakeuptake atat sprucespruce shootshoot andand standstand levellevel
stand
-2
0
2
4
6
8
10
0 250 500 750 1000 1250 1500
PAR, μmol m-2 s-1
AN, μ
mol
m-2
s-1
An_cloudyAn_sunnyFit_cloudyFit_sunny
Ashoot
PossiblePossible caussescausses ofof thethe positive positive effecteffectofof diffusivediffusive radiationradiation on on thethe carboncarbon pumpingpumpingin in thethe forestforest standstand
Solar radation energy penetration into lef interior
Temperature effects
Effects of VPD
Solar radation spectrum within a crown space
Solar radation penetration into crown space
Inclusion of lower crown parts into canopyphotosyntesis
palisade mesophyll spongy mesophyll
CylindricCylindric palisadepalisade cellscells formform effectiveeffective spacespace forfor bebeaamm radiationradiationpenetrationpenetrationSpongySpongy mesophymesophyllll cellcell are are effectivellyeffectivelly illuminatedilluminated by by heterogenousheterogenous diffusivediffusive radiatioradiationn
Solar radation energy penetration into lef interior
Temperature effects
0
5
10
15
20
25
30
35
40
0 0,25 0,5 0,75 1
Time, h
Tair
, °C
Cloudy
Sunny
Typical daily courses of air temperature in sunny and cloudy days
y = 1,2051e0,0937x
R2 = 0,7909
0
2
4
6
8
0 5 10 15 20 25Soil temperature, oC
Soil
CO
2 ef
flux,
um
olC
O 2m-2.s
-1 y = 0,274e0,1167x
R2 = 0,7935
0
1
2
3
4
5
6
0 5 10 15 20 25Cambium temperature, °C
Stem
CO
2 eff
lux,
μm
olC
O 2m
-2s-1
y = 0,1132e0,0919x
R2 = 0,5368
0,0
0,5
1,0
1,5
2,0
2,5
0 5 10 15 20 25 30Leaf temperature, °C
Leaf
resp
irat
ion
, μm
olC
O2
m-2
s-1
The exponential relationships between the rate of CO2 efflux from soil (A), stems (B) and leaves (C) and actual temperature.
Respiration components ofecosystems are exponentiallyrelated to air temperature -
CloudyCloudy daysdays -- frequentlyfrequentlylowerlower airair
temperaturetemperature!!!!!!!!
Effects of VPD
0
1
2
3
4
0:00 6:00 12:00 18:00 0:00
Time, h
VP
D, k
Pa
SunnyCloudy
Typical daily courses of vapour pressure deficit (VPD)over the days with prevailing beam of diffusive radiation
0
50
100
150
200
250
300
0 500 1000 1500 2000
PAR, μmol m-2 s-1
GS,
mm
ol(H
2O) m
-2 s
-1
Gs_cloudyGs_sunny
GsFit-linGsFit-Keen
BThe relationship between stomatal conductivity (GS) and intensity of incident PAR
High value of VPD is relatedto closed stomatal pore -reduction of assimilation
CloudyCloudy daysdays ––frequentlyfrequently lowerlowervaluesvalues ofof VPD!!!!VPD!!!!
Solar radation spectrum within a crown space
Relative photon distribution over the days with prevailing direct (○) and diffuse (●) radiation
Košvancová-Zitová et al.:
Photosynthetica 47: 388-398, 2009
Blue part of solar spectraenhanced stomata openningand is more effective absorbed
CloudyCloudy daysdays ––inductioninduction ofof
asasssimilationimilation!!!!!!!!
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0 10 20 30 40 50
PPFDBlue (μmol m-2 s-1)
GS (
mol
m-2
s-1
)
CloudySunnyFit
C
1.5E-03
2.5E-03
3.5E-03
4.5E-03
400 450 500 550 600 650 700
λ, nm
Rela
tive
phot
on d
istri
butio
n, r
.u.
CloudySunny
StrongStrong differencesdifferences ininBLUEBLUE andand REDRED spectrumspectrum areaarea
Solar radation penetration into crown space
0
25
50
75
100
0 25 50 75 100LAcumul (%)
FAR t
rans
(%)
OblačnoJasno
A
y = 0.602x + 0.95R2 = 0.99
y = 0.800x - 0.23R2 = 0.99
-1
0
1
2
3
4
5
0 2 4 6 8H (m)
Ln(F
AR t
rans
)
OblačnoJasno
B
Relationship between cumulative leaf area (LAcumul) and transmitted photosynthetic photon flux density (PPFDtrans) estimated during sunny (empty circles) and cloudy (full circles) days (A). Slopes of linear relationship between logarithmic PPFDtrans and canopy height H (B). SELA was calculated for incident PPFD 400 μmol m-2 s-1. Empty columns, sunny days; Filled columns, cloudy days.
Diffusive radiation is responsiblefor the lower extinctionscoefficent within crown space
CloudyCloudy daysdays -- ddififfusivefusiveradiationradiation penetratespenetratesdeeperdeeper intointo crowncrownbody !!!body !!!
CloudyCloudy daysdays ––stomatastomata in in thethelowerlower part part ofofthethe crowncrownbody are body are more more openopen!!!!!!
vertical bars indicate 0.95 confidence intervals
sunny
time: 6 8 10 12 13 15 17 19 21-0,05
0,00
0,05
0,10
0,15
0,20
0,25
0,30
0,35
Gs,
mol
m-2
s-1
cloudy
time: 6 8 10 12 13 15 17 19 21
4th whorl 7th whorl 9th whorl 12th whorl
Solar radation penetration into crown space
-20
20
60
100
140
Cloudy Sunny
Am
ount
of C
O 2 a
ssim
ilate
d (g
)
4th whorl7th whorl9th whorl12th whorl
35.8%
12.3%9.4%
42.5%
-4.3%2.1% 24.2%
78.1%
A
CLEAR CLEAR daysdays ––lowerlower crowncrownpartsparts COCO22assimilationassimilationcontributioncontribution isisMINIMAL MINIMAL
CLOUDY CLOUDY daysdays--lowerlower crownscrownspartsparts COCO2 2 assimilationassimilationcontributioncontribution isisINCREASINGINCREASING
Solar radation penetration into crown space
-100
-50
0
50
NEP
[kg
C h
a-1]
-100
-50
0
50
1 2 3 4 5 6 7 8 9 10 11 12
month
NEP
[kg
C h
a-1]
EffectEffect ofof thethe occurenceoccurence ofof solarsolar radiationradiation diffusivediffusive daysdayson on thethe NEP NEP ofof thethe mountainmountain sprucespruce standstand
2005
2007
Majority of „beam“ days
Majority of „diffusive“ days
InterInter--annualannual variationvariation ofof NEP NEP ofof a a sprucespruce forestforest
Kg CO2 ha-1 h-1
2005
-80
-40
0
40
80
120
1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 1.9 1.10 1.11 1.12
NEP
[kgC
ha-1
day
-1]
Carbon depositiondormancy
temp. decreaseovercastovercast + rainsunny + warmovercast + warm
2006
-80
-40
0
40
80
120
1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 1.9 1.10 1.11 1.12
NEP
[kgC
ha-1
day
-1]
2007
-80
-40
0
40
80
120
1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 1.9 1.10 1.11 1.12
NEP
[kgC
ha-1
day
-1]
Deeper analysis of seasonal NEP courses in a mountain spruce forest
EnvironmentalEnvironmental limitslimits ofof thethe biologicalbiological carboncarbon pumpingpumpingin in thethe forestsforests
effecteffect ofof thethe solarsolar radiationradiation typetype
HigherHigher carboncarbon pumpingpumping underunder conditionsconditions ofofdiffusivediffusive radiationradiation isis inducedinduced by:by:
(1) more suitable microclimatological conditions• Air temperture decrease is responsible for respiration decrease,• Decrease of VPD is responsible for stomata oppening,
(2) stimulation of assimilation processes and stomatalconductance because of changes of solar radiation spectralcomposition within the crown space(3) increased radiation penetrartion and thus more significantconnection of lower crown parts into assimilatory activity.
CarbonCarbon pump pump ofof forestforest standstand isis stronglystrongly affectedaffected by by thethe solarsolar diffusivediffusive radiationradiation penetrationpenetration
(1) large part of leaf area is illuminated by the higher radiationexceeding light compensation point – active CO2 sink in largepart of crown space(2) higher proportion of leaf area is an carbon sink for longertime
OthersOthers effectseffects ofof diffusivediffusive radiationradiationWaterWater use use efficiencyefficiency isis INCREASINGINCREASING
stand photosynthesis is responding more significantly to difusiveradiation in comparison to the transpiration
Isoprene Isoprene productionproductionincreased diffusive radiation is connected to the lower volative
compounds production, because of the lower global radiationillumination and thus the lower cooling of stand canopy surface
Knohl A, Baldocchi DD (2008) Effects of diffuse radiation on canopy gas exchange processes in a forest ecosystem. Journal of Geochemical Research, 113, G02023.
EnvironmentalEnvironmental limitslimits ofof thethe biologicalbiological carboncarbon pumpingpumpingin in thethe forestsforests
effecteffect ofof thethe solarsolar radiationradiation typetype