Preprints
https://doi.org/10.5194/egusphere-2026-5529
https://doi.org/10.5194/egusphere-2026-5529
13 Oct 2026
 | 13 Oct 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

A contour-gradient approach for improving glacier centerline extraction in High Mountain Asia

Rongjun Wang, Donghui Shangguan, Wanqin Guo, Shanshan Wang, Dan Zhao, Shijin Wang, Qiudong Zhao, Haidong Han, and Miao Song

Abstract. Glacier centerlines are fundamental to glacier inventory, ice-flow dynamic modeling, and thickness estimation. Although numerous approaches exist for extracting glacier centerlines, they often involve complex processes, require excessive parameters, and produce noticeable deviations, particularly in the accumulation zones of larger glaciers leading to significant discrepancies in subsequent glacier dynamic modeling and thickness estimation. To address this issue, we propose a novel method that extracts glacier centerlines using only a DEM and glacier outlines as input. Our approach integrates contour gradient derived ridge lines and steep terrain constraints to effectively regulate flow direction, while also incorporating a cost grid and hydrological flow routing for enhanced centerline delineation. This approach is characterized by its fully automatic nature, algorithmic simplicity, and high computational efficiency. A total of 134,790 glacier centerlines were derived across High Mountain Asia using our proposed algorithm. Our approach proves effective in extracting centerlines for individual valley glaciers without manual intervention with robust performance even in rugged terrain. The average glacier length is 1.072 km. In total, 607 glaciers in HMA exceed 10 km, and 6 extend beyond 50 km. The longest centerline extracted in our dataset is 82.371 km, corresponding to Siachen Glacier in the Karakoram. We found the centerlines have a good consistency with glacier velocity, indicating it can represent real flow path for glaciers. Our centerlines extraction approach may be beneficial for glacier conceptual models.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Rongjun Wang, Donghui Shangguan, Wanqin Guo, Shanshan Wang, Dan Zhao, Shijin Wang, Qiudong Zhao, Haidong Han, and Miao Song

Status: open (until 24 Nov 2026)

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Rongjun Wang, Donghui Shangguan, Wanqin Guo, Shanshan Wang, Dan Zhao, Shijin Wang, Qiudong Zhao, Haidong Han, and Miao Song
Rongjun Wang, Donghui Shangguan, Wanqin Guo, Shanshan Wang, Dan Zhao, Shijin Wang, Qiudong Zhao, Haidong Han, and Miao Song
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Latest update: 13 Oct 2026
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Short summary
Glacier centerlines are essential for ice flow modeling and ice thickness estimation. Existing methods often fail in the upper parts of large glaciers. We created a simple automatic method using only DEM and glacier outlines. It uses ridges and steep slopes to guide the lines. It was successfully applied to glaciers in High Mountain Asia, and the extracted centerlines agree well with ice velocity. This work helps improve estimates of glacier thickness and future water supply.
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