Preprints
https://doi.org/10.5194/egusphere-2026-4065
https://doi.org/10.5194/egusphere-2026-4065
12 Aug 2026
 | 12 Aug 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Brief communication: Repeated supraglacial lake drainage from the Purepu Glacier system, central Himalaya

Qiangqiang Xu, Shichang Kang, Wentao Du, Wei Wu, Zhaofu Hu, Xiaobo He, Bo Cao, and Biwen Xie

Abstract. We report repeated drainage from the Purepu supraglacial lake system in the central Himalaya using high-resolution satellite imagery. A satellite-inferred 2023 drainage event is constrained to 12–15 July, whereas a reported GLOF occurred early on 8 July 2025. Both followed lake expansion to ~0.70–0.72 km², but DEM-constrained lake-volume loss increased from 0.87 × 10⁶ m³ in 2023 to 3.55 × 10⁶ m³ in 2025. The 2025 event remained incomplete, and flood-volume reconstruction suggests additional englacial or subglacial contributions cannot be excluded. Residual water persisted into 2026, supporting high-frequency monitoring in early July 2026.

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Qiangqiang Xu, Shichang Kang, Wentao Du, Wei Wu, Zhaofu Hu, Xiaobo He, Bo Cao, and Biwen Xie

Status: open (until 03 Oct 2026)

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Qiangqiang Xu, Shichang Kang, Wentao Du, Wei Wu, Zhaofu Hu, Xiaobo He, Bo Cao, and Biwen Xie
Qiangqiang Xu, Shichang Kang, Wentao Du, Wei Wu, Zhaofu Hu, Xiaobo He, Bo Cao, and Biwen Xie

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Short summary
Using frequent high-resolution satellite images, we reconstructed repeated drainage from lakes on the surface of Purepu Glacier in 2023 and 2025. The lakes reached similar sizes before drainage, but the 2025 event released much more water and left substantial residual water into 2026. The results show that lake area alone cannot describe drainage hazard and support intensive monitoring during early to mid-July 2026.
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