Hydrographic investigations in the Irminger Sea in the years 1954-1964

1. The data examined consist of hydrographic sections in the western Irminger Sea and serial observations at Ocean Weather Station Alpha (Station A). The sections were worked in the years 1959 and 1961 -1964, and at station A the data were collected during 5 periods of observation in the years 1954-...

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Main Author: Blindheim, Johan
Format: Report
Language:English
Published: [Fiskeridirektoratets havforskningsinstitutt] 1968
Subjects:
Online Access:http://hdl.handle.net/11250/114648
id ftimr:oai:imr.brage.unit.no:11250/114648
record_format openpolar
spelling ftimr:oai:imr.brage.unit.no:11250/114648 2023-05-15T15:12:23+02:00 Hydrographic investigations in the Irminger Sea in the years 1954-1964 Blindheim, Johan 1968 1035757 bytes application/pdf http://hdl.handle.net/11250/114648 eng eng [Fiskeridirektoratets havforskningsinstitutt] Fiskeridirektoratets skrifter, Serie Havundersøkelser vol 14 no 3 http://hdl.handle.net/11250/114648 s. 72-97 Research report 1968 ftimr 2021-09-23T20:16:10Z 1. The data examined consist of hydrographic sections in the western Irminger Sea and serial observations at Ocean Weather Station Alpha (Station A). The sections were worked in the years 1959 and 1961 -1964, and at station A the data were collected during 5 periods of observation in the years 1954-1963. 2. The sections as well as the data from Station A are used to give the characteristics and extent of different water masses. The occurence of possible annual variations is also examined. 3. South of the Denmark Strait it is difficult to characterize Polar water by means of temperature and salinity, but 34.50 ‰ seems to be the upper limit of its salinity. 4. The intermediate water in the Irminger Sea is found at about 1 000 m depth, and T-S relations for the data from Station A show that the minimum temperature and salinity of intermediate water are 3.5° C and 34.88 ‰. 5. In the Denmark Strait Arctic Intermediate water exhibits temperatures near, or below, 1°C, and salinities chiefly below 34.90 ‰. This water mass seems to be the main source of the bottom water in the Irminger Sea. 6. The amount of Atlantic water which is carried to the Irminger Sea by the Irminger Current, varies from year to year. These variations are studied in the western branch of the Irminger Current and at Station A. In 1954-1956 only small amounts of Atlantic water were observed, but the Atlantic inflow increased until 1959-1960. During the years after 1961 the amount decreased again. 7. At Station A the wind conditions are examined, and there is a close relationship between the accumulated wind and the mean salinity in the different periods of observation. Report Arctic Denmark Strait Institute for Marine Research: Brage IMR Arctic Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054)
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
description 1. The data examined consist of hydrographic sections in the western Irminger Sea and serial observations at Ocean Weather Station Alpha (Station A). The sections were worked in the years 1959 and 1961 -1964, and at station A the data were collected during 5 periods of observation in the years 1954-1963. 2. The sections as well as the data from Station A are used to give the characteristics and extent of different water masses. The occurence of possible annual variations is also examined. 3. South of the Denmark Strait it is difficult to characterize Polar water by means of temperature and salinity, but 34.50 ‰ seems to be the upper limit of its salinity. 4. The intermediate water in the Irminger Sea is found at about 1 000 m depth, and T-S relations for the data from Station A show that the minimum temperature and salinity of intermediate water are 3.5° C and 34.88 ‰. 5. In the Denmark Strait Arctic Intermediate water exhibits temperatures near, or below, 1°C, and salinities chiefly below 34.90 ‰. This water mass seems to be the main source of the bottom water in the Irminger Sea. 6. The amount of Atlantic water which is carried to the Irminger Sea by the Irminger Current, varies from year to year. These variations are studied in the western branch of the Irminger Current and at Station A. In 1954-1956 only small amounts of Atlantic water were observed, but the Atlantic inflow increased until 1959-1960. During the years after 1961 the amount decreased again. 7. At Station A the wind conditions are examined, and there is a close relationship between the accumulated wind and the mean salinity in the different periods of observation.
format Report
author Blindheim, Johan
spellingShingle Blindheim, Johan
Hydrographic investigations in the Irminger Sea in the years 1954-1964
author_facet Blindheim, Johan
author_sort Blindheim, Johan
title Hydrographic investigations in the Irminger Sea in the years 1954-1964
title_short Hydrographic investigations in the Irminger Sea in the years 1954-1964
title_full Hydrographic investigations in the Irminger Sea in the years 1954-1964
title_fullStr Hydrographic investigations in the Irminger Sea in the years 1954-1964
title_full_unstemmed Hydrographic investigations in the Irminger Sea in the years 1954-1964
title_sort hydrographic investigations in the irminger sea in the years 1954-1964
publisher [Fiskeridirektoratets havforskningsinstitutt]
publishDate 1968
url http://hdl.handle.net/11250/114648
long_lat ENVELOPE(-34.041,-34.041,63.054,63.054)
geographic Arctic
Irminger Sea
geographic_facet Arctic
Irminger Sea
genre Arctic
Denmark Strait
genre_facet Arctic
Denmark Strait
op_source s. 72-97
op_relation Fiskeridirektoratets skrifter, Serie Havundersøkelser
vol 14 no 3
http://hdl.handle.net/11250/114648
_version_ 1766343072738705408