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Review of the Melting of West Antarctic Ice Shelves in the Amundsen Sea and Its Influence: Research Issues and Scientific Questions

아문젠해 서남극 빙붕 용융과 영향에 대한 고찰: 연구동향 및 과학적 질문

  • Seung-Tae Yoon (School of Earth System Sciences, College of Natural Sciences, Kyungpook National University)
  • 윤승태 (경북대학교 자연과학대학 지구시스템과학부)
  • Received : 2023.05.23
  • Accepted : 2023.07.09
  • Published : 2023.09.30

Abstract

The collapse of ice shelves is a process that can severely increase the rise of global sea-levels through the reduction of the buttressing effect of ice shelves and the consequent acceleration of the ice flow of ice sheets. In recent years, the West Antarctic ice shelves in the Amundsen Sea, whose buttressing effect is essential for a great part of the West Antarctic ice sheet, have been experiencing the most rapid melting and thinning in the world. The melting of the West Antarctic ice shelves is caused primarily by heat transported by Circumpolar Deep Water (CDW). For this reason, it is important to investigate ice-ocean interactions that could influence the melting of ice shelves and evaluate the stability of West Antarctic ice shelves. A lot of researchers have been actively investigating the West Antarctic ice shelves in the Amundsen Sea. High-impact journals have recognized the importance of and published studies on ice-ocean interactions occurring near and under the ice shelves as well as the connections among ice shelves. However, in situ observations are limited due to extreme weather and sea-ice conditions near the ice shelves; therefore, many scientific questions remain unanswered. This study introduces the characteristics of the Amundsen Sea and investigate the past and latest research issues in this region. This study also gives suggestions regarding important scientific questions and directions for future research that should help early-career scientists take the lead in future research on the melting dynamics of the West Antarctic ice shelves in the Amundsen Sea.

Keywords

Acknowledgement

이 논문은 한국연구재단(NRF-2022R1I1A3063629)과 급격한 남극빙상 용융에 따른 근미래 전지구 해수면 상승예측기술개발(RS-2023-00256677)의 지원을 받아 작성되었습니다.

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