ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA

Aerial observations off East Queen Maud Land, Antarctica, have verified that an open polynya exists and that frazil-ice production occurs there. From the airborne-XBT data, the mixed layer temperature of the polynya attains its freezing point. This polynya is therefore regarded as a latent-heat poly...

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Main Authors: ウシオ シュウキ, タキザワ タカトシ, オオシマ, カワムラ トシユキ, Shuki USHIO, Takatoshi TAKIZAWA, Kay I. OHSHIMA, Toshiyuki KAWAMURA
Format: Report
Language:English
Published: ABSTRACT 1996
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3953
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003953 2023-05-15T13:49:01+02:00 ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA ウシオ シュウキ タキザワ タカトシ オオシマ カワムラ トシユキ Shuki USHIO Takatoshi TAKIZAWA Kay I. OHSHIMA Toshiyuki KAWAMURA 1996-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3953 http://id.nii.ac.jp/1291/00003953/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3953&item_no=1&attribute_id=18&file_no=1 en eng ABSTRACT National Institute of Polar Research Japan Marine Science and Technology Center Institute of Low Temperature Science, Hokkaido University https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3953 http://id.nii.ac.jp/1291/00003953/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 10, 168(1996-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3953&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1996 ftnipr 2022-12-31T19:49:35Z Aerial observations off East Queen Maud Land, Antarctica, have verified that an open polynya exists and that frazil-ice production occurs there. From the airborne-XBT data, the mixed layer temperature of the polynya attains its freezing point. This polynya is therefore regarded as a latent-heat polynya. Thickness of the convective-mixed layer measures 350m or more, which is much deeper than in the offshore pack ice regions. Also, the mixed layer is more homogeneous in salinity profile as compared with those under fast ice regions near Syowa Station. Such a water structure of the polynya suggests active haline convection accompanied by high ice production. Furthermore, the haline convection causes entrainment of the oxygen-poor deep water underlying the winter mixed layer. Thus, the deep-water entrainment decreases the oxygen content of the mixed layer. The average oxygen saturation of the mixed layer in the polynya is 86%, which is almost the same as that of the pack ice region in the Weddell Sea. The oxygen saturation of the deep water is also equal in both regions. However, the mixed-layer thickness of the coastal polynya is much larger than that of the Weddell Sea. This shows that the entrainment rate in the open polynya region is intense. It is estimated that the entrainment rate is three times greater than that in the Weddell Sea. Report Antarc* Antarctic Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology Queen Maud Land Weddell Sea National Institute of Polar Research Repository, Japan Antarctic The Antarctic Weddell Sea Syowa Station Weddell Queen Maud Land ENVELOPE(12.000,12.000,-72.500,-72.500)
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description Aerial observations off East Queen Maud Land, Antarctica, have verified that an open polynya exists and that frazil-ice production occurs there. From the airborne-XBT data, the mixed layer temperature of the polynya attains its freezing point. This polynya is therefore regarded as a latent-heat polynya. Thickness of the convective-mixed layer measures 350m or more, which is much deeper than in the offshore pack ice regions. Also, the mixed layer is more homogeneous in salinity profile as compared with those under fast ice regions near Syowa Station. Such a water structure of the polynya suggests active haline convection accompanied by high ice production. Furthermore, the haline convection causes entrainment of the oxygen-poor deep water underlying the winter mixed layer. Thus, the deep-water entrainment decreases the oxygen content of the mixed layer. The average oxygen saturation of the mixed layer in the polynya is 86%, which is almost the same as that of the pack ice region in the Weddell Sea. The oxygen saturation of the deep water is also equal in both regions. However, the mixed-layer thickness of the coastal polynya is much larger than that of the Weddell Sea. This shows that the entrainment rate in the open polynya region is intense. It is estimated that the entrainment rate is three times greater than that in the Weddell Sea.
format Report
author ウシオ シュウキ
タキザワ タカトシ
オオシマ
カワムラ トシユキ
Shuki USHIO
Takatoshi TAKIZAWA
Kay I. OHSHIMA
Toshiyuki KAWAMURA
spellingShingle ウシオ シュウキ
タキザワ タカトシ
オオシマ
カワムラ トシユキ
Shuki USHIO
Takatoshi TAKIZAWA
Kay I. OHSHIMA
Toshiyuki KAWAMURA
ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA
author_facet ウシオ シュウキ
タキザワ タカトシ
オオシマ
カワムラ トシユキ
Shuki USHIO
Takatoshi TAKIZAWA
Kay I. OHSHIMA
Toshiyuki KAWAMURA
author_sort ウシオ シュウキ
title ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA
title_short ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA
title_full ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA
title_fullStr ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA
title_full_unstemmed ICE PRODUCTION AND CONVECTIVE-MIXING IN THE ANTARCTIC COASTAL POLYNYA
title_sort ice production and convective-mixing in the antarctic coastal polynya
publisher ABSTRACT
publishDate 1996
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3953
http://id.nii.ac.jp/1291/00003953/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3953&item_no=1&attribute_id=18&file_no=1
long_lat ENVELOPE(12.000,12.000,-72.500,-72.500)
geographic Antarctic
The Antarctic
Weddell Sea
Syowa Station
Weddell
Queen Maud Land
geographic_facet Antarctic
The Antarctic
Weddell Sea
Syowa Station
Weddell
Queen Maud Land
genre Antarc*
Antarctic
Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
Queen Maud Land
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
Queen Maud Land
Weddell Sea
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3953
http://id.nii.ac.jp/1291/00003953/
AA10756213
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 10, 168(1996-09)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3953&item_no=1&attribute_id=18&file_no=1
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