Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ...

The Arctic Ocean is connected with the North Atlantic Ocean by the Fram Strait between Greenland and Svalbard. The strait is located in the northern part of the Greenland Sea. In the eastern part of the strait, warm saline water flows northward as the West Spitsbergen Current; while in the western p...

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Main Authors: Ushio, Shuki, Ito, Hajime, Ono, Nobuo
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.701498
https://doi.pangaea.de/10.1594/PANGAEA.701498
id ftdatacite:10.1594/pangaea.701498
record_format openpolar
spelling ftdatacite:10.1594/pangaea.701498 2024-09-15T17:53:58+00:00 Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ... Ushio, Shuki Ito, Hajime Ono, Nobuo 2008 application/zip https://dx.doi.org/10.1594/pangaea.701498 https://doi.pangaea.de/10.1594/PANGAEA.701498 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CTD/Rosette Underway cruise track measurements KF1991 KF1992 KF1993 LA92 LA93/4 SVALB1993a SVALB1993b Boat Lance Polarstar Origo National Polar Research Programme of Japan NIPR article Collection Supplementary Publication Series of Datasets 2008 ftdatacite https://doi.org/10.1594/pangaea.701498 2024-08-01T10:54:23Z The Arctic Ocean is connected with the North Atlantic Ocean by the Fram Strait between Greenland and Svalbard. The strait is located in the northern part of the Greenland Sea. In the eastern part of the strait, warm saline water flows northward as the West Spitsbergen Current; while in the western part, cold less-saline water flows southward as the East Greenland Current. The northwestern part of the Greenland Sea is normally covered with sea ice even in summer. Furthermore, this region is regarded as a major area where the Arctic sea ice is discharged into mid latitude oceans. Thus, this area plays an important role in heat and salt exchange processes in the Arctic marine system.The reveal exchange processes of water masses and ocean-atmosphere interaction in high-latitude oceans, a number of international research programs have been focused on the Greenland Sea and its surrounding waters. As one of the international Arctic research programs, oceanographic studies have been executed in cooperation with the ... : Supplement to: Ushio, Shuki; Ito, Hajime; Ono, Nobuo (1998): Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993. NIPR Arctic Data Reports, National Institute of Polar Research, Tokyo, 3, 46 pp ... Article in Journal/Newspaper Arctic Ocean East Greenland east greenland current Fram Strait Greenland Greenland Sea National Institute of Polar Research North Atlantic Sea ice Svalbard Spitsbergen DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic CTD/Rosette
Underway cruise track measurements
KF1991
KF1992
KF1993
LA92
LA93/4
SVALB1993a
SVALB1993b
Boat
Lance
Polarstar
Origo
National Polar Research Programme of Japan NIPR
spellingShingle CTD/Rosette
Underway cruise track measurements
KF1991
KF1992
KF1993
LA92
LA93/4
SVALB1993a
SVALB1993b
Boat
Lance
Polarstar
Origo
National Polar Research Programme of Japan NIPR
Ushio, Shuki
Ito, Hajime
Ono, Nobuo
Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ...
topic_facet CTD/Rosette
Underway cruise track measurements
KF1991
KF1992
KF1993
LA92
LA93/4
SVALB1993a
SVALB1993b
Boat
Lance
Polarstar
Origo
National Polar Research Programme of Japan NIPR
description The Arctic Ocean is connected with the North Atlantic Ocean by the Fram Strait between Greenland and Svalbard. The strait is located in the northern part of the Greenland Sea. In the eastern part of the strait, warm saline water flows northward as the West Spitsbergen Current; while in the western part, cold less-saline water flows southward as the East Greenland Current. The northwestern part of the Greenland Sea is normally covered with sea ice even in summer. Furthermore, this region is regarded as a major area where the Arctic sea ice is discharged into mid latitude oceans. Thus, this area plays an important role in heat and salt exchange processes in the Arctic marine system.The reveal exchange processes of water masses and ocean-atmosphere interaction in high-latitude oceans, a number of international research programs have been focused on the Greenland Sea and its surrounding waters. As one of the international Arctic research programs, oceanographic studies have been executed in cooperation with the ... : Supplement to: Ushio, Shuki; Ito, Hajime; Ono, Nobuo (1998): Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993. NIPR Arctic Data Reports, National Institute of Polar Research, Tokyo, 3, 46 pp ...
format Article in Journal/Newspaper
author Ushio, Shuki
Ito, Hajime
Ono, Nobuo
author_facet Ushio, Shuki
Ito, Hajime
Ono, Nobuo
author_sort Ushio, Shuki
title Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ...
title_short Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ...
title_full Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ...
title_fullStr Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ...
title_full_unstemmed Oceanographic data in the Greenland Sea and around Svalbard in 1991-1993 ...
title_sort oceanographic data in the greenland sea and around svalbard in 1991-1993 ...
publisher PANGAEA
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.701498
https://doi.pangaea.de/10.1594/PANGAEA.701498
genre Arctic Ocean
East Greenland
east greenland current
Fram Strait
Greenland
Greenland Sea
National Institute of Polar Research
North Atlantic
Sea ice
Svalbard
Spitsbergen
genre_facet Arctic Ocean
East Greenland
east greenland current
Fram Strait
Greenland
Greenland Sea
National Institute of Polar Research
North Atlantic
Sea ice
Svalbard
Spitsbergen
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.701498
_version_ 1810430112270647296