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Precipitation Moisture Source Dataset for the Middle and Lower Reaches of the Yangtze River (26.5°N-33.5°N, 104.5°E-122.5°E) during the Meiyu Season (1991-2020)


ZHANG Chi1HUANG Jinchuan*2,1TANG Qiuhong1XU Ximeng1GAFFNEY Paul P. J.1ZHOU Yuanyuan1
1 Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101,China2 College of Resources and Environmental Sciences,University of Chinese Academy of Sciences,Beijing 100049,China

DOI:10.3974/geodb.2024.07.04.V1

Published:Jul. 2024

Visitors:2477       Data Files Downloaded:23      
Data Downloaded:248.27 MB      Citations:

Key Words:

Meiyu,precipitation,moisture source,middle and lower reaches of the Yangtze River

Abstract:

The precipitation during the Meiyu season (from June to July) has significant implications for droughts, floods, water resource management, and decision-making in the middle and lower reaches of the Yangtze River. Investigating the sources of Meiyu rainfall can help regulate and manage the Meiyu precipitation from its origins. The author used an atmospheric precipitation water vapor tracing numerical model to trace the precipitation in the middle and lower reaches of the Yangtze River (26.5°N-33.5°N, 104.5°E-122.5°E) during the Meiyu season from 1991 to 2020. Then obtained a 30-year distribution of water vapor sources for Meiyu rainfall in the Yangtze River Basin. The model’s driving data were based on observed measurements, and multiple experiments were conducted for comparison and validation, ensuring the reliability of the simulation results. The dataset includes: (1) boundary of the study area; (2) yearly precipitation moisture source during the Meiyu period, with spatial resolution of 1°x1°, and the unit is mm; (3) yearly surface precipitation during the Meiyu period. The dataset is archived in .nc, .shp and .xlsx data formats, and consists of 9 data files with data size of 13.1 MB (Compressed into one file with 10.7 MB). The research results based on this dataset have been published in Weather and Climate Extremes, Vol. 43, 2024.

Foundation Item:

Ministry of Science and Technology of P. R. China (2023YFC3206603); China Scholarship Council (202310490002)

Data Citation:

ZHANG Chi, HUANG Jinchuan*, TANG Qiuhong, XU Ximeng, GAFFNEY Paul P. J., ZHOU Yuanyuan. Precipitation Moisture Source Dataset for the Middle and Lower Reaches of the Yangtze River (26.5°N-33.5°N, 104.5°E-122.5°E) during the Meiyu Season (1991-2020)[J/DB/OL]. Digital Journal of Global Change Data Repository, 2024. https://doi.org/10.3974/geodb.2024.07.04.V1.

References:


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     [7] Zhang, C., Tang, Q., Chen, D. Recent changes in the moisture source of precipitation over the Tibetan Plateau [J]. Journal of Climate, 2017, 30(5): 1807-1819. https://doi.org/10.1175/JCLI-D-15-0842.1.
     [8] Zhang, C., Tang, Q., Chen, D., et al. Moisture source changes contributed to different precipitation changes over the Northern and Southern Tibetan Plateau [J]. Journal of Hydrometeorology, 2019, 20(2): 217-229. https://doi.org/10.1175/JHM-D-18-0094.1.
     [9] Zhang, L., Zhao, D., Zhou, T., et al. Moisture origins and transport processes for the 2020 Yangtze River Valley record-breaking Mei-yu rainfall [J]. Advances in Atmospheric Sciences, 2021(38): 2125-2136.
     

Data Product:

ID Data Name Data Size Operation
1 PrecSourceMLYangtzeRiver1991-2020.rar 11053.49KB
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