Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009

<p>Accurately quantifying the spatiotemporal distribution of the biological component of CO<sub>2</sub> surface–atmosphere exchange is necessary to improve top-down constraints on China's anthropogenic CO<sub>2</sub> emissions. We provide hourly fluxes of CO<...

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Main Authors: A. Dayalu, J. W. Munger, S. C. Wofsy, Y. Wang, T. Nehrkorn, Y. Zhao, M. B. McElroy, C. P. Nielsen, K. Luus
Format: Article
Language:English
Published: Copernicus Publications 2018-11-01
Series:Biogeosciences
Online Access:https://www.biogeosciences.net/15/6713/2018/bg-15-6713-2018.pdf
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author A. Dayalu
A. Dayalu
J. W. Munger
S. C. Wofsy
S. C. Wofsy
Y. Wang
Y. Wang
T. Nehrkorn
Y. Zhao
M. B. McElroy
C. P. Nielsen
K. Luus
author_facet A. Dayalu
A. Dayalu
J. W. Munger
S. C. Wofsy
S. C. Wofsy
Y. Wang
Y. Wang
T. Nehrkorn
Y. Zhao
M. B. McElroy
C. P. Nielsen
K. Luus
author_sort A. Dayalu
collection DOAJ
description <p>Accurately quantifying the spatiotemporal distribution of the biological component of CO<sub>2</sub> surface–atmosphere exchange is necessary to improve top-down constraints on China's anthropogenic CO<sub>2</sub> emissions. We provide hourly fluxes of CO<sub>2</sub> as net ecosystem exchange (NEE; µmol&thinsp;CO<sub>2</sub>&thinsp;m<sup>−2</sup>&thinsp;s<sup>−1</sup>) on a 0.25° × 0.25° grid by adapting the Vegetation, Photosynthesis, and Respiration Model (VPRM) to the eastern half of China for the time period from 2005 to 2009; the minimal empirical parameterization of the VPRM-CHINA makes it well suited for inverse modeling approaches. This study diverges from previous VPRM applications in that it is applied at a large scale to China's ecosystems for the first time, incorporating a novel processing framework not previously applied to existing VPRM versions. In addition, the VPRM-CHINA model prescribes methods for addressing dual-cropping regions that have two separate growing-season modes applied to the same model grid cell. We evaluate the VPRM-CHINA performance during the growing season and compare to other biospheric models. We calibrate the VPRM-CHINA with ChinaFlux and FluxNet data and scale up regionally using Weather Research and Forecasting (WRF) Model v3.6.1 meteorology and MODIS surface reflectances. When combined with an anthropogenic emissions model in a Lagrangian particle transport framework, we compare the ability of VPRM-CHINA relative to an ensemble mean of global hourly flux models (NASA CMS – Carbon Monitoring System) to reproduce observations made at a site in northern China. The measurements are heavily influenced by the northern China administrative region. Modeled hourly time series using vegetation fluxes prescribed by VPRM-CHINA exhibit low bias relative to measurements during the May–September growing season. Compared to NASA CMS subset over the study region, VPRM-CHINA agrees significantly better with measurements. NASA CMS consistently underestimates regional uptake in the growing season. We find that during the peak growing season, when the heavily cropped North China Plain significantly influences measurements, VPRM-CHINA models a CO<sub>2</sub> uptake signal comparable in magnitude to the modeled anthropogenic signal. In addition to demonstrating efficacy as a low-bias prior for top-down CO<sub>2</sub> inventory optimization studies using ground-based measurements, high spatiotemporal resolution models such as the VPRM are critical for interpreting retrievals from global CO<sub>2</sub> remote-sensing platforms such as OCO-2 and OCO-3 (planned). Depending on the satellite time of day and season of crossover, efforts to interpret the relative contribution of the vegetation and anthropogenic components to the measured signal are critical in key emitting regions such as northern China – where the magnitude of the vegetation CO<sub>2</sub> signal is shown to be equivalent to the anthropogenic signal.</p>
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spelling doaj.art-1c470c1b5bbf41c4b174df54c2ba3d022022-12-22T00:06:38ZengCopernicus PublicationsBiogeosciences1726-41701726-41892018-11-01156713672910.5194/bg-15-6713-2018Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009A. Dayalu0A. Dayalu1J. W. Munger2S. C. Wofsy3S. C. Wofsy4Y. Wang5Y. Wang6T. Nehrkorn7Y. Zhao8M. B. McElroy9C. P. Nielsen10K. Luus11Department of Earth and Planetary Sciences, Harvard University, Cambridge, 02138, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, 02138, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, 02138, USADepartment of Earth and Planetary Sciences, Harvard University, Cambridge, 02138, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, 02138, USADepartment of Earth and Atmospheric Sciences, University of Houston, Houston, 77204, USADepartment of Earth System Sciences, Tsinghua University, Beijing, 100084, People's Republic of ChinaAtmospheric and Environmental Research, Inc., Lexington, 02421, USASchool of the Environment, University of Nanjing, Nanjing, 210023, People's Republic of ChinaSchool of Engineering and Applied Sciences, Harvard University, Cambridge, 02138, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, 02138, USACentre for Applied Data Analytics (CeADAR), Dublin 4, Ireland<p>Accurately quantifying the spatiotemporal distribution of the biological component of CO<sub>2</sub> surface–atmosphere exchange is necessary to improve top-down constraints on China's anthropogenic CO<sub>2</sub> emissions. We provide hourly fluxes of CO<sub>2</sub> as net ecosystem exchange (NEE; µmol&thinsp;CO<sub>2</sub>&thinsp;m<sup>−2</sup>&thinsp;s<sup>−1</sup>) on a 0.25° × 0.25° grid by adapting the Vegetation, Photosynthesis, and Respiration Model (VPRM) to the eastern half of China for the time period from 2005 to 2009; the minimal empirical parameterization of the VPRM-CHINA makes it well suited for inverse modeling approaches. This study diverges from previous VPRM applications in that it is applied at a large scale to China's ecosystems for the first time, incorporating a novel processing framework not previously applied to existing VPRM versions. In addition, the VPRM-CHINA model prescribes methods for addressing dual-cropping regions that have two separate growing-season modes applied to the same model grid cell. We evaluate the VPRM-CHINA performance during the growing season and compare to other biospheric models. We calibrate the VPRM-CHINA with ChinaFlux and FluxNet data and scale up regionally using Weather Research and Forecasting (WRF) Model v3.6.1 meteorology and MODIS surface reflectances. When combined with an anthropogenic emissions model in a Lagrangian particle transport framework, we compare the ability of VPRM-CHINA relative to an ensemble mean of global hourly flux models (NASA CMS – Carbon Monitoring System) to reproduce observations made at a site in northern China. The measurements are heavily influenced by the northern China administrative region. Modeled hourly time series using vegetation fluxes prescribed by VPRM-CHINA exhibit low bias relative to measurements during the May–September growing season. Compared to NASA CMS subset over the study region, VPRM-CHINA agrees significantly better with measurements. NASA CMS consistently underestimates regional uptake in the growing season. We find that during the peak growing season, when the heavily cropped North China Plain significantly influences measurements, VPRM-CHINA models a CO<sub>2</sub> uptake signal comparable in magnitude to the modeled anthropogenic signal. In addition to demonstrating efficacy as a low-bias prior for top-down CO<sub>2</sub> inventory optimization studies using ground-based measurements, high spatiotemporal resolution models such as the VPRM are critical for interpreting retrievals from global CO<sub>2</sub> remote-sensing platforms such as OCO-2 and OCO-3 (planned). Depending on the satellite time of day and season of crossover, efforts to interpret the relative contribution of the vegetation and anthropogenic components to the measured signal are critical in key emitting regions such as northern China – where the magnitude of the vegetation CO<sub>2</sub> signal is shown to be equivalent to the anthropogenic signal.</p>https://www.biogeosciences.net/15/6713/2018/bg-15-6713-2018.pdf
spellingShingle A. Dayalu
A. Dayalu
J. W. Munger
S. C. Wofsy
S. C. Wofsy
Y. Wang
Y. Wang
T. Nehrkorn
Y. Zhao
M. B. McElroy
C. P. Nielsen
K. Luus
Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009
Biogeosciences
title Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009
title_full Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009
title_fullStr Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009
title_full_unstemmed Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009
title_short Assessing biotic contributions to CO<sub>2</sub> fluxes in northern China using the Vegetation, Photosynthesis and Respiration Model (VPRM-CHINA) and observations from 2005 to 2009
title_sort assessing biotic contributions to co sub 2 sub fluxes in northern china using the vegetation photosynthesis and respiration model vprm china and observations from 2005 to 2009
url https://www.biogeosciences.net/15/6713/2018/bg-15-6713-2018.pdf
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