Author
Listed:
- Xijia Zhou
(Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center (National Center for Space Weather), China Meteorological Administration, Beijing 100081, China
Innovation Center for the FengYun Meteorological Satellite (FYSIC), Beijing 100081, China)
- Mingwei Zhang
(Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center (National Center for Space Weather), China Meteorological Administration, Beijing 100081, China
Innovation Center for the FengYun Meteorological Satellite (FYSIC), Beijing 100081, China)
- Guicai Li
(Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center (National Center for Space Weather), China Meteorological Administration, Beijing 100081, China
Innovation Center for the FengYun Meteorological Satellite (FYSIC), Beijing 100081, China)
- Yuanyuan Wang
(Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center (National Center for Space Weather), China Meteorological Administration, Beijing 100081, China
Innovation Center for the FengYun Meteorological Satellite (FYSIC), Beijing 100081, China)
- Zhaodi Guo
(Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center (National Center for Space Weather), China Meteorological Administration, Beijing 100081, China
Innovation Center for the FengYun Meteorological Satellite (FYSIC), Beijing 100081, China)
Abstract
Drought events exacerbated by global climate change occur frequently in China. Currently, high-spatiotemporal-resolution gridded meteorological drought index datasets are generally available for single time scales (e.g., 30, 60, 90, and 150 days) and do not fully account for seasonal differences in the impact of drought on vegetation, thus limiting their accuracy when monitoring drought in different regions of China. To compensate for the limitations of existing drought index datasets, a Chinese regional daily meteorological drought comprehensive index (MCI) dataset covering 1951–2022 with a spatial resolution of 0.1 degrees was developed, and standardized precipitation index (SPI) and standardized precipitation evaporation index (SPEI) datasets at 30- and 90-day scales were constructed based on ERA5-Land datasets. Compared with the existing SPI and SPEI datasets, the generated dataset exhibits a high degree of consistency with those in eastern part of China (R 2 > 0.5; the average biases were close to 0 and significantly smaller than RMSEs of the fitting). Additionally, the MCI dataset can more accurately reflect the changes in shallow soil moisture in the eastern part of China in a timely manner (R 2 > 0.7 for the 0–7 cm depth), thus providing notable empirical support for research on drought development in different ecosystems.
Suggested Citation
Xijia Zhou & Mingwei Zhang & Guicai Li & Yuanyuan Wang & Zhaodi Guo, 2025.
"A Database of High-Resolution Meteorological Drought Comprehensive Index Across China for the 1951–2022 Period,"
Data, MDPI, vol. 10(11), pages 1-27, October.
Handle:
RePEc:gam:jdataj:v:10:y:2025:i:11:p:171-:d:1781046
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