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High snow accumulation on Amundsen Sea coastal ice rise, West Antarctica

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Abstract

Polar snow and its accumulation preserve valuable information derived from the atmosphere on past climate and environmental changes in high resolution, particularly in coastal sites. A 2.5-m snow-pit was excavated from the coastal ice rise (Moore Dome) near Amundsen Sea region in February 2012. This study evaluated the isotopic and chemical compositions in the snow-pit and compared them with meteorological variables. Based on the seasonal peaks of the MSA and nssSO42– together with δ18O, δD, and d-excess, the snow-pit record was corresponded to accumulation during austral winter 2011 to summer 2011/2012. The annual mean accumulation rate was assumed thus to be as large as or even higher than 1.03 m w.e. yr–1 at this site. A relatively warm winter temperature in 2011 was traceable in the variations of δ18O, δD, and d-excess. This study emphasizes the importance of the high snow accumulation observed at this site in providing valuable information on sub-annual variations in climate and environmental changes through the study of longer ice cores.

Original languageEnglish
Pages (from-to)365-384
Number of pages20
JournalPolish Polar Research
Volume44
Issue number4
DOIs
StatePublished - 2023

Bibliographical note

Publisher Copyright:
© 2023 Sang-Bum Hong, Yalalt Nyamgerel, Won Sang Lee and Jeonghoon Lee. This is an open access article under the CC BY license http://creativecommons.org/licenses/by/4.0/), which permits use, distribution, and reproduction in any medium, provided that the article is properly cited.

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action

Keywords

  • Antarctica
  • Bear Peninsula
  • Moore Dome
  • snow-pit

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