Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation
This study uses satellite microwave observations to examine the spatiotemporal variations of melting ice sheets on the slopes of Antarctica. These observations were focused on the coastal marginal zone and inland traverse route near Syowa Station. Melting was detected using a 36 GHz vertical polariz...
Published in: | Polar Science |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2020
|
Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16071 http://id.nii.ac.jp/1291/00015952/ |
id |
ftnipr:oai:nipr.repo.nii.ac.jp:00016071 |
---|---|
record_format |
openpolar |
spelling |
ftnipr:oai:nipr.repo.nii.ac.jp:00016071 2023-05-15T13:49:00+02:00 Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation 2020-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16071 http://id.nii.ac.jp/1291/00015952/ en eng https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16071 http://id.nii.ac.jp/1291/00015952/ Polar Science, 25, 100561(2020-09) 18739652 https://doi.org/10.1016/j.polar.2020.100561 Antarctica Ice sheet Melting Rain on snow Microwave observation Journal Article 2020 ftnipr https://doi.org/10.1016/j.polar.2020.100561 2022-12-03T19:43:16Z This study uses satellite microwave observations to examine the spatiotemporal variations of melting ice sheets on the slopes of Antarctica. These observations were focused on the coastal marginal zone and inland traverse route near Syowa Station. Melting was detected using a 36 GHz vertical polarization diurnal amplitude variation (DAV). Data from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) and AMSR2 during 2002–2011 and 2012–2017, respectively, showed DAV variations over time. It was estimated that the greatest melting extent occurred during the 2003/2004 summer; the DAV rose even in the inland areas. In contrast, DAV decreased during rain periods, which was reported by the Japanese Antarctic Research Expedition in 2004 and 2012. This is due to the rise in nighttime brightness temperature (TB). whereas the signal from rain was limited to the lower area. Coastal zones showed a low TB. The low coastal emissions may be attributed to the refrozen ice lenses under the coastal snow layers. The DAV can be significant as the contrast between daytime and nighttime increases from this low TB zone. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Polar Science Polar Science National Institute of Polar Research Repository, Japan Antarctic The Antarctic Syowa Station Polar Science 25 100561 |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
Antarctica Ice sheet Melting Rain on snow Microwave observation |
spellingShingle |
Antarctica Ice sheet Melting Rain on snow Microwave observation Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation |
topic_facet |
Antarctica Ice sheet Melting Rain on snow Microwave observation |
description |
This study uses satellite microwave observations to examine the spatiotemporal variations of melting ice sheets on the slopes of Antarctica. These observations were focused on the coastal marginal zone and inland traverse route near Syowa Station. Melting was detected using a 36 GHz vertical polarization diurnal amplitude variation (DAV). Data from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) and AMSR2 during 2002–2011 and 2012–2017, respectively, showed DAV variations over time. It was estimated that the greatest melting extent occurred during the 2003/2004 summer; the DAV rose even in the inland areas. In contrast, DAV decreased during rain periods, which was reported by the Japanese Antarctic Research Expedition in 2004 and 2012. This is due to the rise in nighttime brightness temperature (TB). whereas the signal from rain was limited to the lower area. Coastal zones showed a low TB. The low coastal emissions may be attributed to the refrozen ice lenses under the coastal snow layers. The DAV can be significant as the contrast between daytime and nighttime increases from this low TB zone. |
format |
Article in Journal/Newspaper |
title |
Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation |
title_short |
Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation |
title_full |
Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation |
title_fullStr |
Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation |
title_full_unstemmed |
Spatiotemporal variation of ice sheet melting in the Antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation |
title_sort |
spatiotemporal variation of ice sheet melting in the antarctic coastal marginal zone and the influence of ice lenses and rain using satellite microwave observation |
publishDate |
2020 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16071 http://id.nii.ac.jp/1291/00015952/ |
geographic |
Antarctic The Antarctic Syowa Station |
geographic_facet |
Antarctic The Antarctic Syowa Station |
genre |
Antarc* Antarctic Antarctica Ice Sheet Polar Science Polar Science |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Polar Science Polar Science |
op_source |
https://doi.org/10.1016/j.polar.2020.100561 |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16071 http://id.nii.ac.jp/1291/00015952/ Polar Science, 25, 100561(2020-09) 18739652 |
op_doi |
https://doi.org/10.1016/j.polar.2020.100561 |
container_title |
Polar Science |
container_volume |
25 |
container_start_page |
100561 |
_version_ |
1766250391822925824 |