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Accuracy evaluation and comparison of GSMaP series for retrieving precipitation on the eastern edge of the Qinghai-Tibet Plateau

Year: 2024
Type: article
Abstract: Min River Basin on the eastern Qinghai-Tibet Plateau. Precipitation is critical for hydrological processes, making accurate data essential for water management and flood forecasting. Satellite precipitation products offer valuable high-resolution spatiotemporal information, with the GSMaP series being widely used. However, comprehensive evaluations of different versions are limited. This study assesses the accuracy of Gauge and MVK products (versions 06, 07, and 08) across spatial and temporal scales and evaluates their performance in detecting precipitation events of varying intensities. (1) GSMaP versions 06 and 07 exhibit higher detection rates for precipitation events, with POD values exceeding 0.8, while version 08 has a lower false alarm rate, with FAR values below 0.15. (2) GSMaP products are more successful in capturing precipitation events during the rainy season than the dry season. (3) With increasing elevation, the Gauge product consistently maintains a high hit rate and reduced false alarm rate, whereas the MVK product's hit rates improve. (4) For different rainfall intensities, GSMaP products more accurately detect moderate and heavy rain events, with the Gauge product outperforming the MVK product in terms of accuracy. These insights enhance the understanding of GSMaP product performance on eastern edge of the Qinghai-Tibet Plateau, aiding in improved water management practices. • GSMaP v06 and 07 show high precipitation accuracy, whereas v08 has low FAR in the eastern edge of QTP. • GSMaP's detection precision ascends with altitude in the eastern edge of QTP, surpassing MVK in Gauge product stability. • GSMaP shows heightened precision in detecting moderate to heavy rainfall in the eastern edge of QTP.
Language: English
Open Access status: gold
Estimated APC paid: $2,460
OpenAlex ID: W4403561764
FWCI: 1.85
Cites: 70
Cited by: 10
Related to: 10