Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, Antarctica

Ice rises and rumples, locally grounded features adjacent to ice shelves, are relatively small yet play significant roles in Antarctic ice dynamics. Their roles generally depend upon their location within the ice shelf and the stage of the ice-sheet retreat or advance. Large, long-stable ice rises c...

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Main Authors: Vikram Goel, Kenichi Matsuoka, Cesar Deschamps Berger, Ian Lee, Jørgen Dall, René Forsberg
Format: Article
Language:English
Published: Cambridge University Press 2020-12-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143020000775/type/journal_article
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author Vikram Goel
Kenichi Matsuoka
Cesar Deschamps Berger
Ian Lee
Jørgen Dall
René Forsberg
author_facet Vikram Goel
Kenichi Matsuoka
Cesar Deschamps Berger
Ian Lee
Jørgen Dall
René Forsberg
author_sort Vikram Goel
collection DOAJ
description Ice rises and rumples, locally grounded features adjacent to ice shelves, are relatively small yet play significant roles in Antarctic ice dynamics. Their roles generally depend upon their location within the ice shelf and the stage of the ice-sheet retreat or advance. Large, long-stable ice rises can be excellent sites for deep ice coring and paleoclimate study of the Antarctic coast and the Southern Ocean, while small ice rises tend to respond more promptly and can be used to reveal recent changes in regional mass balance. The coasts of Dronning Maud Land (DML) and Enderby Land in East Antarctica are abundant with these features. Here we review existing knowledge, presenting an up-to-date status of research in these regions with focus on ice rises and rumples. We use regional datasets (satellite imagery, surface mass balance and ice thickness) to analyze the extent and surface morphology of ice shelves and characteristic timescales of ice rises. We find that large parts of DML have been changing over the past several millennia. Based on our findings, we highlight ice rises suitable for drilling ice cores for paleoclimate studies as well as ice rises suitable for deciphering ice dynamics and evolution in the region.
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spelling doaj.art-f754a599d7984bf4954274e983927b512023-03-09T12:41:00ZengCambridge University PressJournal of Glaciology0022-14301727-56522020-12-01661064107810.1017/jog.2020.77Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, AntarcticaVikram Goel0https://orcid.org/0000-0002-8393-0195Kenichi Matsuoka1https://orcid.org/0000-0002-3587-3405Cesar Deschamps Berger2Ian Lee3https://orcid.org/0000-0001-6871-266XJørgen Dall4https://orcid.org/0000-0002-3873-1074René Forsberg5https://orcid.org/0000-0002-7288-9545National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Vasco-Da-Gama, Goa, India Norwegian Polar Institute, Tromsø, Norway Department of Geosciences, University of Oslo, Oslo, NorwayNorwegian Polar Institute, Tromsø, NorwayNorwegian Polar Institute, Tromsø, Norway Geosciences Department, Ecole Normale Supérieure, 24 rue Lhomond, 75005 Paris, FranceNorwegian Polar Institute, Tromsø, Norway Department of Earth Sciences, University of Washington, Seattle, WA, USATechnical University of Denmark, Lyngby, DenmarkTechnical University of Denmark, Lyngby, DenmarkIce rises and rumples, locally grounded features adjacent to ice shelves, are relatively small yet play significant roles in Antarctic ice dynamics. Their roles generally depend upon their location within the ice shelf and the stage of the ice-sheet retreat or advance. Large, long-stable ice rises can be excellent sites for deep ice coring and paleoclimate study of the Antarctic coast and the Southern Ocean, while small ice rises tend to respond more promptly and can be used to reveal recent changes in regional mass balance. The coasts of Dronning Maud Land (DML) and Enderby Land in East Antarctica are abundant with these features. Here we review existing knowledge, presenting an up-to-date status of research in these regions with focus on ice rises and rumples. We use regional datasets (satellite imagery, surface mass balance and ice thickness) to analyze the extent and surface morphology of ice shelves and characteristic timescales of ice rises. We find that large parts of DML have been changing over the past several millennia. Based on our findings, we highlight ice rises suitable for drilling ice cores for paleoclimate studies as well as ice rises suitable for deciphering ice dynamics and evolution in the region.https://www.cambridge.org/core/product/identifier/S0022143020000775/type/journal_articleAntarctic glaciologyice riseice shelves
spellingShingle Vikram Goel
Kenichi Matsuoka
Cesar Deschamps Berger
Ian Lee
Jørgen Dall
René Forsberg
Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, Antarctica
Journal of Glaciology
Antarctic glaciology
ice rise
ice shelves
title Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, Antarctica
title_full Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, Antarctica
title_fullStr Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, Antarctica
title_full_unstemmed Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, Antarctica
title_short Characteristics of ice rises and ice rumples in Dronning Maud Land and Enderby Land, Antarctica
title_sort characteristics of ice rises and ice rumples in dronning maud land and enderby land antarctica
topic Antarctic glaciology
ice rise
ice shelves
url https://www.cambridge.org/core/product/identifier/S0022143020000775/type/journal_article
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