Preprints
https://doi.org/10.5194/egusphere-2026-1078
https://doi.org/10.5194/egusphere-2026-1078
23 Mar 2026
 | 23 Mar 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Brief communication: Temperature-driven shrinkage of a disappearing Himalayan glacier

Koji Fujita and Rijan B. Kayastha

Abstract. Using drone and GNSS surveys, we updated the geodetic mass balance of Glacier AX010. This glacier has the longest observational record in the Nepal Himalayas, showing accelerating mass loss rates of –1.3 m w.e. a–1 over the last 15 years (2008–2023). We reconstructed 80 years of annual mass balance using a mass-balance model forced by calibrated reanalysis data. While rising temperatures drive shrinkage, changes in precipitation have neither accelerated nor mitigated mass loss. The glacier began losing mass in the early 1970s, accelerated in the early 2000s, and is projected to disappear within one to two decades.

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Koji Fujita and Rijan B. Kayastha

Status: open (until 04 May 2026)

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Koji Fujita and Rijan B. Kayastha
Koji Fujita and Rijan B. Kayastha
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Latest update: 23 Mar 2026
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Short summary
Glacier AX010 in Nepal, monitored since the 1970s, has been shrinking at an accelerating rate, mainly due to rising temperatures. Drone surveys, modeling, and reanalysis data show mass loss began in the early 1970s and intensified after 2000. While rising temperatures drive shrinkage, precipitation changes have neither accelerated nor mitigated mass loss. At the current rate, the glacier may disappear within 10–20 years.
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