Recent giant detachment of a glacier on the Tibetan plateau provoked by its frozen tongue

Abstract Sudden detachments of entire glacier tongues are rare but potentially devastating events that remain poorly understood. Here, we report on an event that occurred in Tibet on November 1, 2022, with an ice volume of ~40 million cubic meters, ranking it among the largest recorded ice avalanches. Utilizing a broad array of satellite data and seismic signals, we reconstruct the motion of the source glacier leading to its failure and the large landscape changes caused by the avalanche. The lack of glacier advance during its acceleration phase suggests that a frozen terminus has played a key role in the evolution of the glacier failure by acting as a dam to the ice mass pushing from above and its potential water content. The dense coverage by satellite data reveals details of an exponential increase in glacier speeds, up to 46 m per day in the weeks and days prior to failure.

Authors

Institutions

Publication Details

Journal
Communications Earth & Environment
Published
2026-01-26
DOI
https://doi.org/10.1038/s43247-025-03125-z
Citations
1
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
40.64
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Recent giant detachment of a glacier on the Tibetan plateau provoked by its frozen tongue

Luc Girod, Désirée Treichler, Andreas Kääb, Juditha Aga et al.
1 citations
Communications Earth & Environment
Cryospheric studies and observations
40.64
article

Recent giant detachment of a glacier on the Tibetan plateau provoked by its frozen tongue

Luc Girod, Désirée Treichler, Andreas Kääb, Juditha Aga, Wei-An Chao
article en
1 citations

Abstract

Abstract Sudden detachments of entire glacier tongues are rare but potentially devastating events that remain poorly understood. Here, we report on an event that occurred in Tibet on November 1, 2022, with an ice volume of ~40 million cubic meters, ranking it among the largest recorded ice avalanches. Utilizing a broad array of satellite data and seismic signals, we reconstruct the motion of the source glacier leading to its failure and the large landscape changes caused by the avalanche. The lack of glacier advance during its acceleration phase suggests that a frozen terminus has played a key role in the evolution of the glacier failure by acting as a dam to the ice mass pushing from above and its potential water content. The dense coverage by satellite data reveals details of an exponential increase in glacier speeds, up to 46 m per day in the weeks and days prior to failure.

Communications Earth & EnvironmentVol. 7(1)
National Yang Ming Chiao Tung University (TW), University of Oslo (NO)
Openalex Percentile: Top 1%
Cryospheric studies and observations
40.64
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.