4.1 Article

Global Terrestrial Ecosystem Carbon Flux Inferred from TanSat XCO2 Retrievals

期刊

JOURNAL OF REMOTE SENSING
卷 2022, 期 -, 页码 -

出版社

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.34133/2022/9816536

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资金

  1. National Key R&D Program of China [2016YFA0600204, SQ2019YFE0 13078]
  2. National Natural Science Foundation of China [41807434, 41907378]
  3. Key Research Program of the Chinese Academy of Sciences [ZDRW-ZS2019-1]

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This study uses the TanSat satellite data to estimate global and regional terrestrial net ecosystem exchange (NEE). The results show an increase in global carbon uptake compared to previous estimates, with a decrease in carbon uptake in northern regions and an increase in carbon release in tropical and southern lands. However, the study also points out that there are biases in the TanSat observations in the northern high latitudes and northern Africa, which need to be addressed for better accuracy in estimates.
TanSat is China's first greenhouse gases observing satellite. In recent years, substantial progresses have been achieved on retrieving column-averaged CO2 dry air mole fraction (XCO2). However, relatively few attempts have been made to estimate terrestrial net ecosystem exchange (NEE) using TanSat XCO2 retrievals. In this study, based on the GEOS-Chem 4D-Var data assimilation system, we infer the global NEE from April 2017 to March 2018 using TanSat XCO2. The inversion estimates global NEE at -3.46 PgC yr(-1), evidently higher than prior estimate and giving rise to an improved estimate of global atmospheric CO2 growth rate. Regionally, our inversion greatly increases the carbon uptakes in northern mid-to-high latitudes and significantly enhances the carbon releases in tropical and southern lands, especially in Africa and India peninsula. The increase of posterior sinks in northern lands is mainly attributed to the decreased carbon release during the nongrowing season, and the decrease of carbon uptakes in tropical and southern lands basically occurs throughout the year. Evaluations against independent CO2 observations and comparison with previous estimates indicate that although the land sinks in the northern middle latitudes and southern temperate regions are improved to a certain extent, they are obviously overestimated in northern high latitudes and underestimated in tropical lands (mainly northern Africa), respectively. These results suggest that TanSat XCO2 retrievals may have systematic negative biases in northern high latitudes and large positive biases over northern Africa, and further efforts are required to remove bias in these regions for better estimates of global and regional NEE.

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