Effect of Assimilating SMAP Soil Moisture on CO2 and CH4 Fluxes through Direct Insertion in a Land Surface Model

نویسندگان

چکیده

Soil moisture impacts the biosphere–atmosphere exchange of CO2 and CH4 plays an important role in terrestrial carbon cycle. A better representation soil would improve coupled carbon–water dynamics ecosystem models could potentially model estimates large-scale fluxes climate feedbacks. Here, we investigate using observations from Moisture Active Passive (SMAP) satellite mission to inform simulated global LPJ-wsl. Results suggest that direct insertion SMAP reduces bias at situ measurement sites by 40%, with a greater improvement temperate sites. wavelet analysis between measurements 26 FLUXNET suggests assimilated run modestly for boreal subtropical 1–2-month time scales. At regional scales, can estimated responses extreme events such as 2018 European drought 2019 rainfall event Sudd (Southern Sudan) wetlands. The improvements land–surface are shown across variety timescales, which potential improving coupling.

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ژورنال

عنوان ژورنال: Remote Sensing

سال: 2022

ISSN: ['2315-4632', '2315-4675']

DOI: https://doi.org/10.3390/rs14102405