Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption
In order to improve quantification of the spatial distribution of carbon sinks and sources in the conterminous US, we conduct a nested global atmospheric inversion with detailed spatial information on crop production and consumption. County-level cropland net primary productivity, harvested biomass,...
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2015-01-01
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doaj-cb022ae383874965a12b135bbeeb6df92020-11-24T22:19:24ZengCopernicus PublicationsBiogeosciences1726-41701726-41892015-01-0112232334310.5194/bg-12-323-2015Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumptionJ. M. Chen0J. W. Fung1G. Mo2F. Deng3T. O. West4International Institute of Earth System Science, Nanjing University, Nanjing, Jiangsu, ChinaDepartment of Geography and Program in Planning, University of Toronto, Toronto, Ontario, M5S 3G3, CanadaDepartment of Geography and Program in Planning, University of Toronto, Toronto, Ontario, M5S 3G3, CanadaDepartment of Physics, University of Toronto, Toronto, Ontario, M5S 3G3, CanadaJoint Global Change Research Institute, Pacific Northwest National Laboratory, College Park, Maryland, USAIn order to improve quantification of the spatial distribution of carbon sinks and sources in the conterminous US, we conduct a nested global atmospheric inversion with detailed spatial information on crop production and consumption. County-level cropland net primary productivity, harvested biomass, soil carbon change, and human and livestock consumption data over the conterminous US are used for this purpose. Time-dependent Bayesian synthesis inversions are conducted based on CO<sub>2</sub> observations at 210 stations to infer CO<sub>2</sub> fluxes globally at monthly time steps with a nested focus on 30 regions in North America. Prior land surface carbon fluxes are first generated using a biospheric model, and the inversions are constrained using prior fluxes with and without adjustments for crop production and consumption over the 2002–2007 period. After these adjustments, the inverted regional carbon sink in the US Midwest increases from 0.25 ± 0.03 to 0.42 ± 0.13 Pg C yr<sup>−1</sup>, whereas the large sink in the US southeast forest region is weakened from 0.41 ± 0.12 to 0.29 ± 0.12 Pg C yr<sup>−1</sup>. These adjustments also reduce the inverted sink in the west region from 0.066 ± 0.04 to 0.040 ± 0.02 Pg C yr<sup>−1</sup> because of high crop consumption and respiration by humans and livestock. The general pattern of sink increases in crop production areas and sink decreases (or source increases) in crop consumption areas highlights the importance of considering the lateral carbon transfer in crop products in atmospheric inverse modeling, which provides a reliable atmospheric perspective of the overall carbon balance at the continental scale but is unreliable for separating fluxes from different ecosystems.http://www.biogeosciences.net/12/323/2015/bg-12-323-2015.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
J. M. Chen J. W. Fung G. Mo F. Deng T. O. West |
spellingShingle |
J. M. Chen J. W. Fung G. Mo F. Deng T. O. West Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption Biogeosciences |
author_facet |
J. M. Chen J. W. Fung G. Mo F. Deng T. O. West |
author_sort |
J. M. Chen |
title |
Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption |
title_short |
Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption |
title_full |
Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption |
title_fullStr |
Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption |
title_full_unstemmed |
Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption |
title_sort |
atmospheric inversion of surface carbon flux with consideration of the spatial distribution of us crop production and consumption |
publisher |
Copernicus Publications |
series |
Biogeosciences |
issn |
1726-4170 1726-4189 |
publishDate |
2015-01-01 |
description |
In order to improve quantification of the spatial distribution of carbon
sinks and sources in the conterminous US, we conduct a nested global
atmospheric inversion with detailed spatial information on crop production
and consumption. County-level cropland net primary productivity, harvested
biomass, soil carbon change, and human and livestock consumption data over
the conterminous US are used for this purpose. Time-dependent Bayesian
synthesis inversions are conducted based on CO<sub>2</sub> observations at 210
stations to infer CO<sub>2</sub> fluxes globally at monthly time steps with a
nested focus on 30 regions in North America. Prior land surface carbon
fluxes are first generated using a biospheric model, and the inversions are
constrained using prior fluxes with and without adjustments for crop
production and consumption over the 2002–2007 period. After these
adjustments, the inverted regional carbon sink in the US Midwest increases
from 0.25 ± 0.03 to 0.42 ± 0.13 Pg C yr<sup>−1</sup>,
whereas the large sink in the US southeast forest region is weakened from
0.41 ± 0.12 to 0.29 ± 0.12 Pg C yr<sup>−1</sup>.
These adjustments also reduce the inverted sink in the west region from
0.066 ± 0.04 to 0.040 ± 0.02 Pg C yr<sup>−1</sup>
because of high crop consumption and respiration by humans and livestock.
The general pattern of sink increases in crop production areas and sink
decreases (or source increases) in crop consumption areas highlights the
importance of considering the lateral carbon transfer in crop products in
atmospheric inverse modeling, which provides a reliable atmospheric
perspective of the overall carbon balance at the continental scale but is
unreliable for separating fluxes from different ecosystems. |
url |
http://www.biogeosciences.net/12/323/2015/bg-12-323-2015.pdf |
work_keys_str_mv |
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