Preprints
https://doi.org/10.5194/egusphere-2025-5199
https://doi.org/10.5194/egusphere-2025-5199
24 Nov 2025
 | 24 Nov 2025
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Tracking In-Situ Snow Accumulation at Neumayer, Coastal Antarctica: Signs of Climatic Changes in the past 30 Years?

Valerie Reppert, Olaf Eisen, Holger Schmithüsen, Stefanie Arndt, Guido Ascenso, Linda Ort, and Zsófia Jurányi

Abstract. This study investigates monthly snow accumulation derived from in-situ measurements at Neumayer Station, coastal Dronning Maud Land, East Antarctica, over a 33-year period (1991–2024). Snow accumulation is the major component of the surface mass balance, which is among the most uncertain factors of Antarctica's contribution to global sea level rise. The analysis aims to (1) quantify seasonal contributions and detect climatological shifts, (2) compare annual accumulation rates across three measurement sites, and (3) investigate the magnitude and nature of interannual variability. Results reveal high intra- and interannual variability without a consistent seasonal cycle. Out of the four seasons, only the austral autumn season has shown a statistically significant increase in accumulation over the past 30 years. Although no robust long-term trend was detected in annual accumulation rates, the years 2021 and 2023 stand out as statistically rare positive extremes observed across the measurement sites. Spectral analyses reveal pronounced interannual to decadal variability, which hinders the detection of potential trends and raises the question of whether these extremes reflect constructive interference of natural variability modes or indicate the onset of a regime shift in accumulation driven by global climate warming. Supplementary analysis of monthly average meteorological parameters (temperature, relative humidity, and wind fields) revealed no consistent link to accumulation on monthly scales, suggesting a decoupling between local meteorology and snow accumulation at these time scales. This highlights the need for further research into short-term processes and event-scale accumulation drivers. The datasets presented here provide a long-term base for validating regional climate models and for ground-truthing remote sensing products related to Antarctic snow accumulation and surface mass balance.

Competing interests: At least one of the (co-)authors is a member of the editorial board of The Cryosphere.

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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Valerie Reppert, Olaf Eisen, Holger Schmithüsen, Stefanie Arndt, Guido Ascenso, Linda Ort, and Zsófia Jurányi

Status: open (until 05 Jan 2026)

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Valerie Reppert, Olaf Eisen, Holger Schmithüsen, Stefanie Arndt, Guido Ascenso, Linda Ort, and Zsófia Jurányi

Data sets

High resolved snow height measurements at Neumayer Station, Antarctica (2010 et seq) Schmithüsen, H. https://doi.org/10.1594/PANGAEA.958970

Time series of accumulation measurements from stake farm Neumayer Pegelfeld Süd,610 Ekström Ice Shelf, Antarctica, since 1991 Eisen, O., Reppert, V., Weller, R., and Jurányi, Z. https://doi.org/10.1594/PANGAEA.972104

Continuous meteorological observations at Neumayer station (1982-03 et seq), Schmithüsen, H. https://doi.org/10.1594/PANGAEA.962313

Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2013S2, deployed during Antarctic Fast Ice Network 2013 (AFIN 2013) Nicolaus, M. and Hoppmann, M. https://doi.org/10.1594/PANGAEA.887807

Valerie Reppert, Olaf Eisen, Holger Schmithüsen, Stefanie Arndt, Guido Ascenso, Linda Ort, and Zsófia Jurányi
Metrics will be available soon.
Latest update: 24 Nov 2025
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Short summary
We analyzed 33 years of snow accumulation measurements at Neumayer Station, Antarctica, to understand changes in the amount of snow building up on the surface over time. The long-term, high-resolution data show mostly stable accumulation, but rare positive extremes appeared in 2021 and 2023. Seasonal and multi-year patterns were identified, providing valuable data to improve climate models and satellite observations.
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