On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica

Characteristics of sea ice variations in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica, have been described with satellite data archived since the 1970s. In the Indian Ocean sector, the period of maximum ice extent is generally reached in October, a month later than in other sectors....

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Main Author: Shuki Ushio
Format: Article
Language:English
Published: National Institute of Polar Research 2006-07-01
Series:Antarctic Record
Online Access:http://doi.org/10.15094/00009364
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author Shuki Ushio
author_facet Shuki Ushio
author_sort Shuki Ushio
collection DOAJ
description Characteristics of sea ice variations in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica, have been described with satellite data archived since the 1970s. In the Indian Ocean sector, the period of maximum ice extent is generally reached in October, a month later than in other sectors. The probable reason for the delay is eastward sea-ice drift from the Weddell Sea sector west of the Indian Ocean sector. During the ice melt season, the highest rate of ice retreat from November to December appears in the Indian Ocean sector. Also, the ice edge along 40 degrees east longitude off Lutzow-Holmbukta shows a remarkable delay pattern at the beginning of autumn ice extent season and rapid retreat of the ice edge in the spring melt season. These features are qualitatively explainable due to Cosmonaut Polynya formation.
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spelling doaj.art-622c4b7dc7af4809b0b8b46b4510c70e2022-12-22T02:30:01ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X2006-07-0150214215110.15094/00009364On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, AntarcticaShuki Ushio0National Institute of Polar ResearchCharacteristics of sea ice variations in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica, have been described with satellite data archived since the 1970s. In the Indian Ocean sector, the period of maximum ice extent is generally reached in October, a month later than in other sectors. The probable reason for the delay is eastward sea-ice drift from the Weddell Sea sector west of the Indian Ocean sector. During the ice melt season, the highest rate of ice retreat from November to December appears in the Indian Ocean sector. Also, the ice edge along 40 degrees east longitude off Lutzow-Holmbukta shows a remarkable delay pattern at the beginning of autumn ice extent season and rapid retreat of the ice edge in the spring melt season. These features are qualitatively explainable due to Cosmonaut Polynya formation.http://doi.org/10.15094/00009364
spellingShingle Shuki Ushio
On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica
Antarctic Record
title On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica
title_full On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica
title_fullStr On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica
title_full_unstemmed On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica
title_short On sea-ice advance and retreat in the Indian Ocean sector and off Lutzow-Holmbukta, Antarctica
title_sort on sea ice advance and retreat in the indian ocean sector and off lutzow holmbukta antarctica
url http://doi.org/10.15094/00009364
work_keys_str_mv AT shukiushio onseaiceadvanceandretreatintheindianoceansectorandofflutzowholmbuktaantarctica