TY - JOUR
T1 - Linking global terrestrial CO2 fluxes and environmental drivers
T2 - Inferences from the Orbiting Carbon Observatory 2 satellite and terrestrial biospheric models
AU - Chen, Zichong
AU - Liu, Junjie
AU - Henze, Daven K.
AU - Huntzinger, Deborah N.
AU - Wells, Kelley C.
AU - Sitch, Stephen
AU - Friedlingstein, Pierre
AU - Joetzjer, Emilie
AU - Bastrikov, Vladislav
AU - Goll, Daniel S.
AU - Haverd, Vanessa
AU - Jain, Atul K.
AU - Kato, Etsushi
AU - Lienert, Sebastian
AU - Lombardozzi, Danica L.
AU - Mcguire, Patrick C.
AU - Melton, Joe R.
AU - Nabel, Julia E.M.S.
AU - Poulter, Benjamin
AU - Tian, Hanqin
AU - Wiltshire, Andrew J.
AU - Zaehle, Sönke
AU - Miller, Scot M.
N1 - Publisher Copyright:
© Author(s) 2021.
PY - 2021/5/4
Y1 - 2021/5/4
N2 - Observations from the Orbiting Carbon Observatory 2 (OCO-2) satellite have been used to estimate CO2 fluxes in many regions of the globe and provide new insight into the global carbon cycle. The objective of this study is to infer the relationships between patterns in OCO-2 observations and environmental drivers (e.g., temperature, precipitation) and therefore inform a process understanding of carbon fluxes using OCO-2. We use a multiple regression and inverse model, and the regression coefficients quantify the relationships between observations from OCO-2 and environmental driver datasets within individual years for 2015- 2018 and within seven global biomes.We subsequently compare these inferences to the relationships estimated from 15 terrestrial biosphere models (TBMs) that participated in the TRENDY model inter-comparison. Using OCO-2, we are able to quantify only a limited number of relationships between patterns in atmospheric CO2 observations and patterns in environmental driver datasets (i.e., 10 out of the 42 relationships examined). We further find that the ensemble of TBMs exhibits a large spread in the relationships with these key environmental driver datasets. The largest uncertainty in the models is in the relationship with precipitation, particularly in the tropics, with smaller uncertainties for temperature and photosynthetically active radiation (PAR). Using observations from OCO-2, we find that precipitation is associated with increased CO2 uptake in all tropical biomes, a result that agrees with half of the TBMs. By contrast, the relationships that we infer from OCO-2 for temperature and PAR are similar to the ensemble mean of the TBMs, though the results differ from many individual TBMs. These results point to the limitations of current space-based observations for inferring environmental relationships but also indicate the potential to help inform key relationships that are very uncertain in stateof- the-art TBMs.
AB - Observations from the Orbiting Carbon Observatory 2 (OCO-2) satellite have been used to estimate CO2 fluxes in many regions of the globe and provide new insight into the global carbon cycle. The objective of this study is to infer the relationships between patterns in OCO-2 observations and environmental drivers (e.g., temperature, precipitation) and therefore inform a process understanding of carbon fluxes using OCO-2. We use a multiple regression and inverse model, and the regression coefficients quantify the relationships between observations from OCO-2 and environmental driver datasets within individual years for 2015- 2018 and within seven global biomes.We subsequently compare these inferences to the relationships estimated from 15 terrestrial biosphere models (TBMs) that participated in the TRENDY model inter-comparison. Using OCO-2, we are able to quantify only a limited number of relationships between patterns in atmospheric CO2 observations and patterns in environmental driver datasets (i.e., 10 out of the 42 relationships examined). We further find that the ensemble of TBMs exhibits a large spread in the relationships with these key environmental driver datasets. The largest uncertainty in the models is in the relationship with precipitation, particularly in the tropics, with smaller uncertainties for temperature and photosynthetically active radiation (PAR). Using observations from OCO-2, we find that precipitation is associated with increased CO2 uptake in all tropical biomes, a result that agrees with half of the TBMs. By contrast, the relationships that we infer from OCO-2 for temperature and PAR are similar to the ensemble mean of the TBMs, though the results differ from many individual TBMs. These results point to the limitations of current space-based observations for inferring environmental relationships but also indicate the potential to help inform key relationships that are very uncertain in stateof- the-art TBMs.
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U2 - 10.5194/acp-21-6663-2021
DO - 10.5194/acp-21-6663-2021
M3 - Article
AN - SCOPUS:85105516962
SN - 1680-7316
VL - 21
SP - 6663
EP - 6680
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 9
ER -