The glacial geomorphology of western Dronning Maud Land, Antarctica

Reconstructing the response of present-day ice sheets to past global climate change is important for constraining and refining the numerical models which forecast future contributions of these ice sheets to sea-level change. Mapping landforms is an essential step in reconstructing glacial histories....

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Main Authors: J. C. H. Newall, T. Dymova, E. Serra, R. Blomdin, O. Fredin, N. F. Glasser, Y. Suganuma, J. M. Harbor, A. P. Stroeven
Format: Article
Language:English
Published: Taylor & Francis Group 2020-12-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2020.1761464
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spelling doaj-4a200a7203154a63a059e8737384b9ce2021-01-15T13:32:55ZengTaylor & Francis GroupJournal of Maps1744-56472020-12-0116246847810.1080/17445647.2020.17614641761464The glacial geomorphology of western Dronning Maud Land, AntarcticaJ. C. H. Newall0T. Dymova1E. Serra2R. Blomdin3O. Fredin4N. F. Glasser5Y. Suganuma6J. M. Harbor7A. P. Stroeven8Geomorphology & Glaciology, Department of Physical Geography, Stockholm UniversityGeomorphology & Glaciology, Department of Physical Geography, Stockholm UniversityGeomorphology & Glaciology, Department of Physical Geography, Stockholm UniversityGeomorphology & Glaciology, Department of Physical Geography, Stockholm UniversityGeological Survey of NorwayCentre for Glaciology, Department of Geography and Earth Sciences, Aberystwyth UniversityNational Institute of Polar ResearchGeomorphology & Glaciology, Department of Physical Geography, Stockholm UniversityGeomorphology & Glaciology, Department of Physical Geography, Stockholm UniversityReconstructing the response of present-day ice sheets to past global climate change is important for constraining and refining the numerical models which forecast future contributions of these ice sheets to sea-level change. Mapping landforms is an essential step in reconstructing glacial histories. Here we present a new map of glacial landforms and deposits on nunataks in western Dronning Maud Land, Antarctica. Nunataks are mountains or ridges that currently protrude through the ice sheet and may provide evidence that they have been wholly or partly covered by ice, thus indicating a formerly more extensive (thicker) ice sheet. The map was produced through a combination of mapping from Worldview satellite imagery and ground validation. The sub-metre spatial resolution of the satellite imagery enabled mapping with unprecedented detail. Ten landform categories have been mapped, and the landform distributions provide evidence constraining spatial patterns of a previously thicker ice sheet.http://dx.doi.org/10.1080/17445647.2020.1761464antarcticaglacial geomorphologynunatakpaleoglaciologyworldview
collection DOAJ
language English
format Article
sources DOAJ
author J. C. H. Newall
T. Dymova
E. Serra
R. Blomdin
O. Fredin
N. F. Glasser
Y. Suganuma
J. M. Harbor
A. P. Stroeven
spellingShingle J. C. H. Newall
T. Dymova
E. Serra
R. Blomdin
O. Fredin
N. F. Glasser
Y. Suganuma
J. M. Harbor
A. P. Stroeven
The glacial geomorphology of western Dronning Maud Land, Antarctica
Journal of Maps
antarctica
glacial geomorphology
nunatak
paleoglaciology
worldview
author_facet J. C. H. Newall
T. Dymova
E. Serra
R. Blomdin
O. Fredin
N. F. Glasser
Y. Suganuma
J. M. Harbor
A. P. Stroeven
author_sort J. C. H. Newall
title The glacial geomorphology of western Dronning Maud Land, Antarctica
title_short The glacial geomorphology of western Dronning Maud Land, Antarctica
title_full The glacial geomorphology of western Dronning Maud Land, Antarctica
title_fullStr The glacial geomorphology of western Dronning Maud Land, Antarctica
title_full_unstemmed The glacial geomorphology of western Dronning Maud Land, Antarctica
title_sort glacial geomorphology of western dronning maud land, antarctica
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2020-12-01
description Reconstructing the response of present-day ice sheets to past global climate change is important for constraining and refining the numerical models which forecast future contributions of these ice sheets to sea-level change. Mapping landforms is an essential step in reconstructing glacial histories. Here we present a new map of glacial landforms and deposits on nunataks in western Dronning Maud Land, Antarctica. Nunataks are mountains or ridges that currently protrude through the ice sheet and may provide evidence that they have been wholly or partly covered by ice, thus indicating a formerly more extensive (thicker) ice sheet. The map was produced through a combination of mapping from Worldview satellite imagery and ground validation. The sub-metre spatial resolution of the satellite imagery enabled mapping with unprecedented detail. Ten landform categories have been mapped, and the landform distributions provide evidence constraining spatial patterns of a previously thicker ice sheet.
topic antarctica
glacial geomorphology
nunatak
paleoglaciology
worldview
url http://dx.doi.org/10.1080/17445647.2020.1761464
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