COS: A new tracer to constrain photosynthetic CO2 fluxes Dan Yakir 1 , Max Berkelhammer 2 , Hulin Chen 2 J. Miller 3 1 Environmental Sciences and Energy Research, Weizmann Institute NOAA-GMD, Boulder, 3 CIREES, UC Boulder 29/5/2014 5th Kaplan, Sdot-Yam 1
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COS: A new tracer to constrain photosynthetic CO2 fluxes
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COS: A new tracer to constrain photosynthetic CO2 fluxes
Dan Yakir1,
Max Berkelhammer2, Hulin Chen2 J. Miller3 1Environmental Sciences and Energy Research, Weizmann Institute
NOAA-GMD, Boulder, 3CIREES, UC Boulder
29/5/2014 5th Kaplan, Sdot-Yam 1
29/5/2014 5th Kaplan, Sdot-Yam 2
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A greatest sources of uncertainty for future climate predictions Is the response of the global carbon cycle to climate change
…our mass balance analysis shows that net global carbon uptake has increased significantly by about 0.05 Gt C per year and that g lobal carbon uptake doubled, from 2.4±0.8 to 5.0±0.9 Gt per year between 1960 and 2010… Ballantyne et al 2012
NEE = GPP + Re
GPP Re
Net CO2 flux
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A major limitation: we cannot measure photosynthesis above the leaf scale
Soil uptake (74-180)
Anthropogenic, direct/indirect (90-266)
Direct COS (110-190) Indirect CS2, DMS (149-330)
Unknown (~600)
Stratosphere COSàSO2 OH uptake (82-110)
Global COS Budget (Gg S a-1; Kettle et al., 2002; Montzka et al., 2007; Berry et al., 2013 )
Mean atmospheric concentration ~500 ppt!
Leaf uptake (730-1500)
?
Global ocean
BB, wetland (81-119)
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COS Uptake by Leaf During Photosynthesis
COS
CO2
COS and CO2 are taken up through leaf stomata during
photosynthesis
CO2
COS
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Exiting new technological advances (Quantum cascade, mid IR lasers, Mobile lab….
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GPP
Ra
NPP
CO2 into leaves
Rh
NEE COS
Changes in ratio of COS to CO2 uptake across scales