Simulated monthly runoff at Pasighat over the Yarlung Zangbo basin (2018-2019)

2024-02-23 22:50:25 WEBDHM 4
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The Third Pole experiences accelerated glacier retreating particularly in the easternHimalaya, coinciding with a decrease of monsoon-precipitation in the early 21st century. In the lower reaches of Yarlung Zangbo basin, both of glacier melting and rainfall are rich, but the contribution to the surface runoff and the impact is unknown. The extent to which the vanishing abundant maritime glaciers buffer the declining precipitation-runoff in the upstream of upper Brahmaputra basin (UBB) remains unclear. With a state-of-the-art enthalpy-based distributed cryosphere-hydrology model and first-hand hydrometeorology observations at Motuo (latest accessible Chinese county), we carefully examine hydrological processes in the Yarlung Zangbo basin along Himalayas.
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201801-201912.xlsx
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Reference of data

Wang, L. (2022). Simulated monthly runoff at Pasighat over the Yarlung Zangbo basin (2018-2019). National Tibetan Plateau / Third Pole Environment Data Center. https://doi.org/10.11888/Terre.tpdc.300103. https://cstr.cn/18406.11.Terre.tpdc.300103.

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Article citation

1、Wang, Y., Wang, L., Zhou, J., Yao, T., Yang, W., Zhong, X., Liu, R., Hu, Z., Luo, L., Ye, Q., Chen, N., & Ding, H. (2021). Vanishing Glaciers at Southeast Tibetan Plateau Have Not Offset the Declining Runoff at Yarlung Zangbo. Geophysical Research Letters, 48(21), e2021GL094651. https://doi.org/10.1029/2021GL094651 ( View details Bibtex )

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Funded project

1、 Strategic Priority Research Program (A) of the Chinese Academy of Sciences ：Pan-Third Pole Environment Study for a Green Silk Road-A CAS Strategic Priority A Program（XDA20000000）

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