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Sökning: WFRF:(Chen Weimin) > (2020-2024) > China's Terrestrial...

China's Terrestrial Carbon Sink Over 2010–2015 Constrained by Satellite Observations of Atmospheric CO2 and Land Surface Variables

He, Wei (författare)
Nanjing University
Jiang, Fei (författare)
Nanjing University
Wu, Mousong (författare)
Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science,Nanjing University
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Ju, Weimin (författare)
Nanjing University
Scholze, Marko (författare)
Lund University,Lunds universitet,BECC: Biodiversity and Ecosystem services in a Changing Climate,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,MERGE: ModElling the Regional and Global Earth system,Institutionen för naturgeografi och ekosystemvetenskap,Centre for Environmental and Climate Science (CEC),Faculty of Science,Dept of Physical Geography and Ecosystem Science
Chen, Jing M. (författare)
Byrne, Brendan (författare)
California Institute of Technology
Liu, Junjie (författare)
California Institute of Technology
Wang, Hengmao (författare)
Nanjing University
Wang, Jun (författare)
Nanjing University
Wang, Songhan (författare)
Nanjing Agricultural University
Zhou, Yanlian (författare)
Nanjing University
Zhang, Chunhua (författare)
Nguyen, Ngoc Tu (författare)
Hohai University
Shen, Yang (författare)
Nanjing University
Chen, Zhi (författare)
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 (creator_code:org_t)
2022
2022
Engelska.
Ingår i: Journal of Geophysical Research: Biogeosciences. - 2169-8953. ; 127:2
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The magnitude and distribution of China's terrestrial carbon sink remain uncertain due to insufficient constraints at large scales, whereby satellite data offer great potential for reducing the uncertainty. Here, we present two carbon sink estimates for China constrained either by satellite CO2 column concentrations (XCO2) within the Global Carbon Assimilation System or by remotely sensed soil moisture and Fraction of Absorbed Photosynthetically Active Radiation (FAPAR) in addition to in situ CO2 observations within the Carbon Cycle Data Assimilation System. They point to a moderate size of carbon sinks of 0.34 ± 0.14 (mean ± unc.) and 0.43 ± 0.09 PgC/yr during 2010–2015, which are supported by an inventory-based estimate for forest and soil carbon sink (0.26 PgC/yr) and fall in the range of contemporary ensemble atmospheric inversions (0.25–0.48 PgC/yr). They also agree reasonably well on interannual variations, which reflect the carbon sink anomalies induced by regional droughts in southwest China. Furthermore, their spatial distributions are broadly consistent that of the forest inventory-based estimate, indicating that the largest carbon sinks locate in central and eastern China. Their estimates for forest carbon sink coincide fairly well with the inventory-based estimate across different regions, especially when aggregated to the north and south of China. Although enhanced recently by afforestation, China's carbon sink was also significantly weakened by regional droughts, which were often not fully represented in previous in situ CO2-based inversions due to insufficient observations. Our results suggest that satellite-based atmospheric CO2 and land surface observations are vital in characterizing terrestrial net carbon fluxes at regional scales.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

Nyckelord

atmospheric CO concentration
atmospheric inversion
China's carbon sink
data assimilation
multisource satellite observations

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