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Fusion of Surface Soil Moisture Data for Spatial Downscaling of Daily Satellite Precipitation Data

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Published
<mark>Journal publication date</mark>31/01/2024
<mark>Journal</mark>IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
Volume17
Number of pages13
Pages (from-to)1053-1065
Publication StatusPublished
Early online date28/11/23
<mark>Original language</mark>English

Abstract

Remote sensing satellites provide an effective solution for obtaining large-scale precipitation data. However, the spatial resolution of satellite-based precipitation products is often too coarse for hydrological applications at the regional scale. As a solution, spatial downscaling has been increasingly investigated to increase the spatial resolution of satellite-based precipitation. The selection of effective explanatory variables at fine spatial resolution has become a crucial concern in precipitation downscaling. Generally, surface soil moisture (SSM) has a strong physical relation with precipitation (especially at the regional scale), but this relationship has rarely been considered. In this article, we proposed to fuse SSM in precipitation downscaling. Specifically, the 3 km SSM data (i.e., SPL2SMAP_S) were incorporated to downscale the 10 km Integrated Multisatellite Retrievals for Global Precipitation Measurement daily precipitation data to 3 km. Based on case studies in southeastern China, the proposed strategy was compared with the existing scheme fusing digital elevation model or normalized difference vegetation index data as an alternative. The results demonstrated that, compared to the original precipitation product, all downscaling results can provide richer spatial details. The proposed scheme outperformed the other schemes, with a correlation coefficient of 0.63, a root-mean-square error of 15.7 mm, and a mean absolute error of 8.74 mm. Furthermore, the proposed scheme is more sensitive to precipitation events of different intensities. In addition, when the historical precipitation is discontinuous, the advantages of the proposed scheme are more apparent.