TY - JOUR
T1 - Critical land change information enhances the understanding of carbon balance in the United States
AU - Liu, Jinxun
AU - Sleeter, Benjamin M.
AU - Zhu, Zhiliang
AU - Loveland, Thomas R.
AU - Sohl, Terry
AU - Howard, Stephen M.
AU - Key, Carl H.
AU - Hawbaker, Todd
AU - Liu, Shuguang
AU - Reed, Bradley
AU - Cochrane, Mark A.
AU - Heath, Linda S.
AU - Jiang, Hong
AU - Price, David T.
AU - Chen, Jing M.
AU - Zhou, Decheng
AU - Bliss, Norman B.
AU - Wilson, Tamara
AU - Sherba, Jason
AU - Zhu, Qiuan
AU - Luo, Yiqi
AU - Poulter, Benjamin
N1 - Publisher Copyright:
© 2020 John Wiley & Sons Ltd
PY - 2020/7/1
Y1 - 2020/7/1
N2 - Large-scale terrestrial carbon (C) estimating studies using methods such as atmospheric inversion, biogeochemical modeling, and field inventories have produced different results. The goal of this study was to integrate fine-scale processes including land use and land cover change into a large-scale ecosystem framework. We analyzed the terrestrial C budget of the conterminous United States from 1971 to 2015 at 1-km resolution using an enhanced dynamic global vegetation model and comprehensive land cover change data. Effects of atmospheric CO2 fertilization, nitrogen deposition, climate, wildland fire, harvest, and land use/land cover change (LUCC) were considered. We estimate annual C losses from cropland harvest, forest clearcut and thinning, fire, and LUCC were 436.8, 117.9, 10.5, and 10.4 TgC/year, respectively. C stored in ecosystems increased from 119,494 to 127,157 TgC between 1971 and 2015, indicating a mean annual net C sink of 170.3 TgC/year. Although ecosystem net primary production increased by approximately 12.3 TgC/year, most of it was offset by increased C loss from harvest and natural disturbance and increased ecosystem respiration related to forest aging. As a result, the strength of the overall ecosystem C sink did not increase over time. Our modeled results indicate the conterminous US C sink was about 30% smaller than previous modeling studies, but converged more closely with inventory data.
AB - Large-scale terrestrial carbon (C) estimating studies using methods such as atmospheric inversion, biogeochemical modeling, and field inventories have produced different results. The goal of this study was to integrate fine-scale processes including land use and land cover change into a large-scale ecosystem framework. We analyzed the terrestrial C budget of the conterminous United States from 1971 to 2015 at 1-km resolution using an enhanced dynamic global vegetation model and comprehensive land cover change data. Effects of atmospheric CO2 fertilization, nitrogen deposition, climate, wildland fire, harvest, and land use/land cover change (LUCC) were considered. We estimate annual C losses from cropland harvest, forest clearcut and thinning, fire, and LUCC were 436.8, 117.9, 10.5, and 10.4 TgC/year, respectively. C stored in ecosystems increased from 119,494 to 127,157 TgC between 1971 and 2015, indicating a mean annual net C sink of 170.3 TgC/year. Although ecosystem net primary production increased by approximately 12.3 TgC/year, most of it was offset by increased C loss from harvest and natural disturbance and increased ecosystem respiration related to forest aging. As a result, the strength of the overall ecosystem C sink did not increase over time. Our modeled results indicate the conterminous US C sink was about 30% smaller than previous modeling studies, but converged more closely with inventory data.
KW - DGVM
KW - carbon sequestration
KW - ecosystem model
KW - ecosystem productivity
KW - land use and land cover change
KW - wildfire
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U2 - 10.1111/gcb.15079
DO - 10.1111/gcb.15079
M3 - Article
C2 - 32162439
AN - SCOPUS:85083388393
SN - 1354-1013
VL - 26
SP - 3920
EP - 3929
JO - Global change biology
JF - Global change biology
IS - 7
ER -