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Section 1: Publication
Publication Type
Journal Article
Authorship
Lu, X., Tang, G., Wang, X., Liu, Y., Wei, M., & Zhang, Y.
Title
The Development of a Two-Step Merging and Downscaling Method for Satellite Precipitation Products
Year
2020
Publication Outlet
Remote Sensing, 12(3), 398
DOI
ISBN
ISSN
Citation
Lu, X., Tang, G., Wang, X., Liu, Y., Wei, M., & Zhang, Y. (2020). The Development of a Two-Step Merging and Downscaling Method for Satellite Precipitation Products. Remote Sensing, 12(3), 398.
https://doi.org/10.3390/rs12030398
Abstract
Low accuracy and coarse spatial resolution are the two main drawbacks of satellite precipitation products. Therefore, calibration and downscaling are necessary before these products are applied. This study proposes a two-step framework to improve the accuracy of satellite precipitation estimates. The first step is data merging based on optimum interpolation (OI), and the second step is downscaling based on geographically weighted regression (GWR); therefore, the framework is called OI-GWR. An Integrated Multi-satellitE Retrievals for Global Precipitation Measurement (GPM) (IMERG) product is used to demonstrate the effectiveness of OI-GWR in the Tianshan Mountains, China. First, the original IMERG precipitation data (OIMERG) are merged with rain gauge data using the OI method to produce corrected IMERG precipitation data (CIMERG). Then, using CIMERG as the first guess and the normalized difference vegetation index (NDVI) as the auxiliary variable, GWR is utilized for spatial downscaling. The two-step OI-GWR method is compared with several traditional methods, including GWR downscaling (Ori_GWR) and spline interpolation. The cross-validation results show that (1) the OI method noticeably improves the accuracy of OIMERG, and (2) the 1-km downscaled data obtained using OI-GWR are much better than those obtained from Ori_GWR, spline interpolation, and OIMERG. The proposed OI-GWR method can contribute to the development of high-resolution and high-accuracy regional precipitation datasets. However, it should be noted that the method proposed in this study cannot be applied in regions without any meteorological stations. In addition, further efforts will be needed to achieve daily- or hourly-scale downscaling of precipitation.
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