Rare ice-base temperature measurements in Antarctica reveal a cold base in contrast with predictions

The Antarctic bed demonstrates complex behaviour comprising alternating warm- and cold-based areas. However, the distribution of warm- and cold-based areas, basal melting rates, and the structure and age of the basal ice are not yet fully known. In the 2023–2024 season, we drilled an access borehole through 541 m thick ice at Princess Elizabeth Land, 28 km south of the coast. Temperature measurements at the bottom of the borehole revealed a cold underlying base despite a warm-based interface being predicted in advance as the most likely estimate. Our results imply that the Antarctic base can be locally colder than currently assumed, and that thermal models, especially basal boundary conditions, should be carefully specified and provided with the confirmed input data. Temperature measurements at bedrock below 541 meters of ice in Antarctica’s Princess Elizabeth Land show a cold base with basal ice solidly frozen to the bedrock, in contrast with advance predictions of a warm bed, as found in an access borehole in 2024.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-03-08
DOI
https://doi.org/10.1038/s43247-025-02127-1
Citations
6
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
7.80

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article

Rare ice-base temperature measurements in Antarctica reveal a cold base in contrast with predictions

Yuchen Sun, Yazhuo Li, Pavel G. Тalalay, И. Б. Абдрахманов et al.
6 citations
Communications Earth & Environment
Cryospheric studies and observations
7.80
article

Rare ice-base temperature measurements in Antarctica reveal a cold base in contrast with predictions

Yuchen Sun, Yazhuo Li, Pavel G. Тalalay, И. Б. Абдрахманов, Da Gong, Andrey N. Salamatin, M.A. Vorobyev, Alexey Ekaykin, German Leitchenkov, V. Lipenkov, Xiaopeng Fan, Bing Li, Nan Zhang, Youhong Sun, Yunchen Liu, Damir Khalimov
article en
6 citations

Abstract

The Antarctic bed demonstrates complex behaviour comprising alternating warm- and cold-based areas. However, the distribution of warm- and cold-based areas, basal melting rates, and the structure and age of the basal ice are not yet fully known. In the 2023–2024 season, we drilled an access borehole through 541 m thick ice at Princess Elizabeth Land, 28 km south of the coast. Temperature measurements at the bottom of the borehole revealed a cold underlying base despite a warm-based interface being predicted in advance as the most likely estimate. Our results imply that the Antarctic base can be locally colder than currently assumed, and that thermal models, especially basal boundary conditions, should be carefully specified and provided with the confirmed input data. Temperature measurements at bedrock below 541 meters of ice in Antarctica’s Princess Elizabeth Land show a cold base with basal ice solidly frozen to the bedrock, in contrast with advance predictions of a warm bed, as found in an access borehole in 2024.

Communications Earth & EnvironmentVol. 6(1)
Jilin University (CN), Arctic and Antarctic Research Institute (RU), China University of Geosciences (Beijing) (CN), All Russian Research Institute of Geology and Mineral Resources of the World Ocean (RU), Institute of Geography (RU), Jilin Province Science and Technology Department (CN)
National Natural Science Foundation of China
Climate action
Openalex Percentile: Top 2%
Cryospheric studies and observations
7.80
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