The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland

All available data on bathymetry, temperature, salinity and currents up until and including 1975 are used in describing the seasonal changes and dynamics of the hydrography of Disko Bugt, the Vaigat and adjacent glacier and non glacier fjords. From a winter situation with well mixed -1.75°C cold wat...

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Main Author: Andersen, Ole G. Norden
Format: Article in Journal/Newspaper
Language:English
Published: Danish Polar Center/Museum Tusculanum Press 1981
Subjects:
Online Access:https://tidsskrift.dk/meddrgroenland_biosci/article/view/142180
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spelling ftsbaarhusojs:oai:ojs.tidsskrift.dk:article/142180 2024-01-28T10:04:38+01:00 The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland Andersen, Ole G. Norden 1981-08-28 application/pdf https://tidsskrift.dk/meddrgroenland_biosci/article/view/142180 eng eng Danish Polar Center/Museum Tusculanum Press https://tidsskrift.dk/meddrgroenland_biosci/article/view/142180/185874 https://tidsskrift.dk/meddrgroenland_biosci/article/view/142180 Meddelelser om Grønland. Bioscience; Vol. 5 (1981): Meddelelser om Grønland. Bioscience; 33 pp. Meddelelser om Grønland. Bioscience; Årg. 5 (1981): Meddelelser om Grønland. Bioscience; 33 pp. 0106-1054 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1981 ftsbaarhusojs 2024-01-03T23:59:24Z All available data on bathymetry, temperature, salinity and currents up until and including 1975 are used in describing the seasonal changes and dynamics of the hydrography of Disko Bugt, the Vaigat and adjacent glacier and non glacier fjords. From a winter situation with well mixed -1.75°C cold water in the upper c. 100 m steep halo-and thermoclines develop during the summer between freshened and heated surface water leaving Disko Bugt and deeper more saline water entering from the West Greenland Current. Huge ice bergs have a decisive cooling effect upon the upper 150-200 m affecting the outflowing current as well as the inflowing water which is responsible for the high bottom temperatures and salinities (up to 3.5°C and 34-34.5‰ at 300-500 m) found the year round, and which contributes to raising the temperature in the upper 200 m in the summer, especially in the southern and eastern part of the bay and even into the Vaigat. Surface temperatures reach 12°C in the offshore waters of the bay where salinities may drop to 30‰, and inshore in the more diluted waters of Disko Fjord temperatures may even reach 14°C, whereas in the glacier fjords, where surface salinities come close to zero, 4°C is the highest temperature recorded and subzero temperatures are found even in July. An extensive upwelling of W Greenland water occurs in the northern part of the bay during the summer and fall and similar phenomena occur in Disko Fjord, driven by winds and apparently linked to tidal rhythms. Although TS diagrams show that deep Disko Bugt water and Baffin Bay water is of common origin, no water seems to enter Disko Bugt from Baffin Bay or from the Baffin Current. Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Disko bugt glacier Greenland Aarhus University: OJS at The State and University Library Baffin Bay Greenland Vaigat ENVELOPE(-52.947,-52.947,70.200,70.200)
institution Open Polar
collection Aarhus University: OJS at The State and University Library
op_collection_id ftsbaarhusojs
language English
description All available data on bathymetry, temperature, salinity and currents up until and including 1975 are used in describing the seasonal changes and dynamics of the hydrography of Disko Bugt, the Vaigat and adjacent glacier and non glacier fjords. From a winter situation with well mixed -1.75°C cold water in the upper c. 100 m steep halo-and thermoclines develop during the summer between freshened and heated surface water leaving Disko Bugt and deeper more saline water entering from the West Greenland Current. Huge ice bergs have a decisive cooling effect upon the upper 150-200 m affecting the outflowing current as well as the inflowing water which is responsible for the high bottom temperatures and salinities (up to 3.5°C and 34-34.5‰ at 300-500 m) found the year round, and which contributes to raising the temperature in the upper 200 m in the summer, especially in the southern and eastern part of the bay and even into the Vaigat. Surface temperatures reach 12°C in the offshore waters of the bay where salinities may drop to 30‰, and inshore in the more diluted waters of Disko Fjord temperatures may even reach 14°C, whereas in the glacier fjords, where surface salinities come close to zero, 4°C is the highest temperature recorded and subzero temperatures are found even in July. An extensive upwelling of W Greenland water occurs in the northern part of the bay during the summer and fall and similar phenomena occur in Disko Fjord, driven by winds and apparently linked to tidal rhythms. Although TS diagrams show that deep Disko Bugt water and Baffin Bay water is of common origin, no water seems to enter Disko Bugt from Baffin Bay or from the Baffin Current.
format Article in Journal/Newspaper
author Andersen, Ole G. Norden
spellingShingle Andersen, Ole G. Norden
The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland
author_facet Andersen, Ole G. Norden
author_sort Andersen, Ole G. Norden
title The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland
title_short The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland
title_full The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland
title_fullStr The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland
title_full_unstemmed The annual cycle of temperature, salinity, currents and water masses in Disko Bugt and adjacent waters, West Greenland
title_sort annual cycle of temperature, salinity, currents and water masses in disko bugt and adjacent waters, west greenland
publisher Danish Polar Center/Museum Tusculanum Press
publishDate 1981
url https://tidsskrift.dk/meddrgroenland_biosci/article/view/142180
long_lat ENVELOPE(-52.947,-52.947,70.200,70.200)
geographic Baffin Bay
Greenland
Vaigat
geographic_facet Baffin Bay
Greenland
Vaigat
genre Baffin Bay
Baffin Bay
Baffin
Disko bugt
glacier
Greenland
genre_facet Baffin Bay
Baffin Bay
Baffin
Disko bugt
glacier
Greenland
op_source Meddelelser om Grønland. Bioscience; Vol. 5 (1981): Meddelelser om Grønland. Bioscience; 33 pp.
Meddelelser om Grønland. Bioscience; Årg. 5 (1981): Meddelelser om Grønland. Bioscience; 33 pp.
0106-1054
op_relation https://tidsskrift.dk/meddrgroenland_biosci/article/view/142180/185874
https://tidsskrift.dk/meddrgroenland_biosci/article/view/142180
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