Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region
Ice-free areas cover a small percentage of the land in the South Shetland Islands. However, they are significant as they contain ecosystems highly sensitive to environmental changes and are located within a region affected by global warming. These areas are dominated by periglacial, glacial, fluvial...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5003884 2023-05-15T14:02:23+02:00 Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region López-Martínez, J. Schmid, T. Serrano, E. Mink, S. Nieto, A. Guillaso, S. 2016 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5003884 eng eng info:eu-repo/semantics/altIdentifier/doi/10.18172/cig.2965 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5003884 Cuadernos de Investigacion Geografica info:eu-repo/semantics/article 2016 ftgfzpotsdam https://doi.org/10.18172/cig.2965 2022-09-14T05:57:25Z Ice-free areas cover a small percentage of the land in the South Shetland Islands. However, they are significant as they contain ecosystems highly sensitive to environmental changes and are located within a region affected by global warming. These areas are dominated by periglacial, glacial, fluvial, and coastal processes and landforms, where permafrost is often present. Soil development is observed although vegetation cover is sparse and closely related to the geomorphology. The mapping and monitoring of ice-free areas is important as they are highly sensitive to climate change. The objective of this study was to characterize and map surface landforms in ice-free areas using traditional mapping methods as well as advanced remote sensing techniques. Geomorphological and topographical maps were initially obtained through field measurements and observations, and complemented with existing aerial photography at scales between 1:2000 and 1:25000. Thereafter, satellite-borne data became available and were included in the methodology to further determine the distribution of the landforms. In the Antarctic environment, Synthetic Aperture Radar (SAR) provides the most reliable images as data can be obtained in any weather conditions as well as during the day and night. Fully polarimetric SAR RADARSAT-2 were used to determine seven different terrain classes representing surface landforms in ice-free areas around Maxwell Bay (King George Island). The SAR remote sensing techniques were successfully applied to identify different periglacial, fluvial, glacial, coastal, as well as lithological landforms. Field data from Fildes Peninsula were used to train a supervised classifier to map further areas around Maxwell Bay. In this case, the ice-free areas around Maxwell Bay clearly show the dominance of periglacial landforms and processes. Therefore, these techniques can be used to compare past and future results and to monitor areas affected by changing environmental factors and increasing human activities. Article in Journal/Newspaper Antarc* Antarctic Ice King George Island Maxwell Bay permafrost South Shetland Islands GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Antarctic The Antarctic King George Island South Shetland Islands Fildes ENVELOPE(-58.817,-58.817,-62.217,-62.217) Fildes peninsula ENVELOPE(-58.948,-58.948,-62.182,-62.182) Maxwell Bay ENVELOPE(-58.859,-58.859,-62.223,-62.223) Cuadernos de Investigación Geográfica 42 2 435 |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
Ice-free areas cover a small percentage of the land in the South Shetland Islands. However, they are significant as they contain ecosystems highly sensitive to environmental changes and are located within a region affected by global warming. These areas are dominated by periglacial, glacial, fluvial, and coastal processes and landforms, where permafrost is often present. Soil development is observed although vegetation cover is sparse and closely related to the geomorphology. The mapping and monitoring of ice-free areas is important as they are highly sensitive to climate change. The objective of this study was to characterize and map surface landforms in ice-free areas using traditional mapping methods as well as advanced remote sensing techniques. Geomorphological and topographical maps were initially obtained through field measurements and observations, and complemented with existing aerial photography at scales between 1:2000 and 1:25000. Thereafter, satellite-borne data became available and were included in the methodology to further determine the distribution of the landforms. In the Antarctic environment, Synthetic Aperture Radar (SAR) provides the most reliable images as data can be obtained in any weather conditions as well as during the day and night. Fully polarimetric SAR RADARSAT-2 were used to determine seven different terrain classes representing surface landforms in ice-free areas around Maxwell Bay (King George Island). The SAR remote sensing techniques were successfully applied to identify different periglacial, fluvial, glacial, coastal, as well as lithological landforms. Field data from Fildes Peninsula were used to train a supervised classifier to map further areas around Maxwell Bay. In this case, the ice-free areas around Maxwell Bay clearly show the dominance of periglacial landforms and processes. Therefore, these techniques can be used to compare past and future results and to monitor areas affected by changing environmental factors and increasing human activities. |
format |
Article in Journal/Newspaper |
author |
López-Martínez, J. Schmid, T. Serrano, E. Mink, S. Nieto, A. Guillaso, S. |
spellingShingle |
López-Martínez, J. Schmid, T. Serrano, E. Mink, S. Nieto, A. Guillaso, S. Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region |
author_facet |
López-Martínez, J. Schmid, T. Serrano, E. Mink, S. Nieto, A. Guillaso, S. |
author_sort |
López-Martínez, J. |
title |
Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region |
title_short |
Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region |
title_full |
Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region |
title_fullStr |
Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region |
title_full_unstemmed |
Geomorphology and landforms distribution in selected ice-free areas in the South Shetland Islands, Antarctic Northern Peninsula region |
title_sort |
geomorphology and landforms distribution in selected ice-free areas in the south shetland islands, antarctic northern peninsula region |
publishDate |
2016 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5003884 |
long_lat |
ENVELOPE(-58.817,-58.817,-62.217,-62.217) ENVELOPE(-58.948,-58.948,-62.182,-62.182) ENVELOPE(-58.859,-58.859,-62.223,-62.223) |
geographic |
Antarctic The Antarctic King George Island South Shetland Islands Fildes Fildes peninsula Maxwell Bay |
geographic_facet |
Antarctic The Antarctic King George Island South Shetland Islands Fildes Fildes peninsula Maxwell Bay |
genre |
Antarc* Antarctic Ice King George Island Maxwell Bay permafrost South Shetland Islands |
genre_facet |
Antarc* Antarctic Ice King George Island Maxwell Bay permafrost South Shetland Islands |
op_source |
Cuadernos de Investigacion Geografica |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.18172/cig.2965 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5003884 |
op_doi |
https://doi.org/10.18172/cig.2965 |
container_title |
Cuadernos de Investigación Geográfica |
container_volume |
42 |
container_issue |
2 |
container_start_page |
435 |
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1766272654180876288 |