Randomized trial evaluates rainfall variability and gridded datasets in the Tibetan Plateau, suggesting improvements for data accuracy.
Study region The Zayu River Basin in the southeastern Tibetan Plateau. Study focus Utilizing a dense network of 18 newly deployed rain gauges, this study characterizes spatiotemporal rainfall variability and evaluates six gridded precipitation products. We integrated multi-scale assessments (daily to hourly) with an event-based error decomposition framework to diagnose systematic biases in satellite and reanalysis datasets. New hydrological insights for the region: Observations reveal early-morning rainfall peaks and substantial spatial heterogeneity. At the daily scale, gauge-based CHM (China Hydro-Meteorology Precipitation) outperforms others. For all the hourly products, evaluations expose a distinct spatial disparity: western tributaries exhibit higher detection skill, while eastern tributaries suffer severe overestimation. Specifically, GMCP (Global Multisource Merging-and-Calibration Precipitation) proves most robust. Error decomposition reveals that ERA5-Land (the land component of the fifth-generation ECMWF atmospheric reanalysis) biases stem from "drizzle effects" (false-end errors), whereas IMERG (Integrated Multi-satellite Retrievals for Global Precipitation Measurement) biases arise from stochastic detection failures (miss-events). These diagnostics offer critical guidance for correcting precipitation data in data-scarce alpine regions.
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Li et al. (2026) studied this question.
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