Evidence map›Paper›PMID 41398331›Full record

ArticleScientific reports2025

Evaluating multi-source precipitation data for streamflow simulation using the SWAT model in the Alpine Manas River Basin, Northwest China.

Li Tan, Chanjuan Zan, Tie Liu, Jiayu Xiong, Aoxiang Zhang

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Article in Scientific reports, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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5 · Who and what money

Authors and funding

5 authors.

Li TanSchool of Geophysics, Chengdu University of Technology, Chengdu, 610059, China.
Chanjuan ZanSchool of Geographical Sciences, China West Normal University, Nanchong, 637009, Sichuan, China. zanchanjuan@cwnu.edu.cn.
Tie LiuCollege of Geoinformatics, Zhejiang University of Technology, Hangzhou, 310014, China.
Jiayu XiongSchool of Geophysics, Chengdu University of Technology, Chengdu, 610059, China.
Aoxiang ZhangSchool of Geophysics, Chengdu University of Technology, Chengdu, 610059, China.

Funding

Key R&D Program of Xinjiang Uygur Autonomous Region 2022B03021-2Sichuan Science and Technology Program 2023YFN0022
6 · The paper itself

Abstract

Due to the influence of topography, climate, and other factors, the applicability of precipitation products varies significantly across different regions. Investigating the differences among multi-source precipitation products and their suitability for streamflow simulation in cold and alpine basins not only helps to reveal the advantages and limitations of each product but also plays an important role in improving the accuracy and application of hydrological models. Combining comprehensive indexes for precipitation magnitude and precipitation event detection capability, and the SWAT model, this study compares and analyzes the accuracy of four precipitation products (CMFD, MSWEP, ERA5-LAND, IMERG) in the arid regions of Xinjiang and explores their applicability in streamflow simulation for the alpine Manas River Basin. All four products demonstrate consistent intra-annual precipitation variation patterns. Significant discrepancies emerge specifically during summer. IMERG yields the lowest precipitation estimates, underestimating monthly totals with underestimations reaching approximately 39% to 45.7% in spring and autumn. Conversely, IMERG overestimates precipitation by 6.43% to 35.2% in July and August. Both CMFD and MSWEP underestimate precipitation during the rainy season while overestimating it in the dry season. The annual mean precipitation is overestimated by 4.05% to 6.59%. ERA5-Land exhibits a substantial overall overestimation of approximately 45.6%. CMFD demonstrates optimal overall precipitation performance with higher station correlation and relatively stable behavior across precipitation intensity levels. MSWEP and ERA5-Land exhibit comparable performance, though MSWEP shows smaller daily-scale biases than CMFD. MSWEP-based daily streamflow simulations yielded optimal results, achieving Nash-Sutcliffe Efficiency (NSE) > 0.65 during both calibration and validation periods with PBIAS < 15%. CMFD and ERA5-Land generated similar streamflow simulations, consistently overestimating streamflow by 12.79 ~ 27.07% in both periods. This study offers valuable references for streamflow simulation and water resource management in data-scarce alpine basins.

Indexed as

Adaptability assessmentAlpine basinHydrological modelPrecipitation productsStreamflow simulation

Identifiers

PMID41398331
PMCPMC12705700

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.