Soil Moisture Assimilation Improves Terrestrial Biosphere Model GPP Responses to Sub-Annual Drought at Continental Scale

Author:

Xing Xiuli1,Wu Mousong12,Scholze Marko2ORCID,Kaminski Thomas3,Vossbeck Michael3,Lu Zhengyao2,Wang Songhan4,He Wei1,Ju Weimin1,Jiang Fei15ORCID

Affiliation:

1. International Institute for Earth System Science, Nanjing University, Nanjing 210023, China

2. Department of Physical Geography and Ecosystem Science, Lund University, SE-22362 Lund, Sweden

3. The Inversion Lab, 20249 Hamburg, Germany

4. College of Agriculture, Nanjing Agricultural University, Nanjing 210095, China

5. Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China

Abstract

Due to the substantial gross exchange fluxes with the atmosphere, the terrestrial carbon cycle plays a significant role in the global carbon budget. Drought commonly affects terrestrial carbon absorption negatively. Terrestrial biosphere models exhibit significant uncertainties in capturing the carbon flux response to drought, which have an impact on estimates of the global carbon budget. Through plant physiological processes, soil moisture tightly regulates the carbon cycle in the environment. Therefore, accurate observations of soil moisture may enhance the modeling of carbon fluxes in a model–data fusion framework. We employ the Carbon Cycle Data Assimilation System (CCDAS) to assimilate 36-year satellite-derived surface soil moisture observations in combination with flask samples of atmospheric CO2 concentrations. We find that, compared to the default model, the performance of optimized net ecosystem productivity (NEP) and gross primary productivity (GPP) has increased with the RMSEs reduced by 1.62 gC/m2/month and 10.84 gC/m2/month, which indicates the added value of the ESA-CCI soil moisture observations as a constraint on the terrestrial carbon cycle. Additionally, the combination of soil moisture and CO2 concentration in this study improves the representation of inter-annual variability of terrestrial carbon fluxes as well as the atmospheric CO2 growth rate. We thereby investigate the ability of the optimized GPP in responding to drought by comparing continentally aggregated GPP with the drought index. The assimilation of surface soil moisture has been shown to efficiently capture the influences of the sub-annual (≤9 months drought durations) and large-scale (e.g., regional to continental scales) droughts on GPP. This study highlights the significant potential of satellite soil moisture for constraining inter-annual models of the terrestrial biosphere’s carbon cycle and for illustrating how GPP responds to drought at a continental scale.

Funder

National Key Research and Development Program of China

National Natural Science Foundation of China

Research Funds for the Frontiers Science Center for Critical Earth Material Cycling, Nanjing University

Swedish National Space Board

ESA SMOS+VEGETATION

Land surface Carbon Constellation

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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