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  • Institut für Meereskunde  (5)
  • Blackwell Publishing Ltd  (1)
  • Hamburg : Leitstelle Meteor, Inst. für Meereskunde der Univ. Hamburg  (1)
  • 1
    Book
    Book
    Hamburg : Leitstelle Meteor, Inst. für Meereskunde der Univ. Hamburg
    Type of Medium: Book
    Pages: II, 105 S , Ill., graph. Darst., Kt
    Series Statement: Meteor-Berichte 93,1
    Language: English
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  • 2
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Heat and freshwater transports through Fram Strait are understood to have a significant influence on the hydrographic conditions in the Arctic Ocean and on water mass modifications in the Nordic seas. To determine these transports and their variability reliable estimates of the volume transport through the strait are required. Current meter moorings were deployed in Fram Strait from September 1997 to September 1999 in the framework of the EU MAST III Variability of Exchanges in the Northern Seas programme. The monthly mean velocity fields reveal marked velocity variations over seasonal and annual time scales, and the spatial structure of the northward flowing West Spitsbergen Current and the southward East Greenland Current with a maximum in spring and a minimum in summer. The volume transport obtained by averaging the monthly means over two years amounts to 9.5 ± 1.4 Sv to the north and 11.1 ± 1.7 Sv to the south (1 Sv = 106 m3s−1). The West Spitsbergen Current has a strong barotropic and a weaker baroclinic component; in the East Greenland Current barotropic and baroclinic components are of similar magnitude. The net transport through the strait is 4.2 ± 2.3 Sv to the south. The obtained northward and southward transports are significantly larger than earlier estimates in the literature; however, within its range of uncertainty the balance obtained from a two year average is consistent with earlier estimates.
    Type of Medium: Electronic Resource
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  • 3
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    Institut für Meereskunde
    In:  Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, 119 . Institut für Meereskunde, Kiel, Germany, 68 pp.
    Publication Date: 2016-09-08
    Type: Report , NonPeerReviewed
    Format: text
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  • 4
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    Institut für Meereskunde
    In:  Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, 134 . Institut für Meereskunde, Kiel, Germany, 60 pp.
    Publication Date: 2014-12-12
    Type: Report , NonPeerReviewed
    Format: text
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  • 5
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    Institut für Meereskunde
    In:  Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, 146 . Institut für Meereskunde, Kiel, Germany, 80 pp.
    Publication Date: 2019-09-23
    Type: Report , NonPeerReviewed
    Format: text
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  • 6
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    Institut für Meereskunde
    In:  Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, 118 . Institut für Meereskunde, Kiel, Germany, 90 pp.
    Publication Date: 2015-10-06
    Type: Report , NonPeerReviewed
    Format: text
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  • 7
    Publication Date: 2022-04-22
    Description: Es werden die Daten des Polarfront-Programms während des Internationalen Geophysikalischen Jahres 1957/58 verwendet, um die Frage des Eindringens jahresperiodischer Oberflächenstörungen zu untersuchen. Nach der Diskussion der Oberflächenstörungen und der bei der Ermittlung der Eindringtiefe auftretenden Fehler werden durch den Vergleich von TS-Kurven die gesuchten Tiefenwerte gefunden. Für das Seegebiet südöstlich Grönlands wird eine spezielle Untersuchung durchgeführt. Unter stark vereinfachten Verhältnissen werden vertikale Austauschkoeffizienten ermittelt. Zum Abschluß wird die Frage untersucht, wieweit die für das Jahr 1958 gefundenen Verhältnisse repräsentativ für das Untersuchungsgebiet sind. Data of the "Polar Front Survey", one of the most extensive oceanographic programs during the International Geophysical Year 1957/58, were used to determine the maximum depth of penetration of seasonal surface disturbances. The area of investigation covers the North Atlantic between 40°N-65°N and 10°W-45°W. It is established, that next to the annual water budget and the annual cycle of windspeed, the heat budget is the most important factor causing variations of yearly periods in deeper layers. The maximum depth of penetration is determined by comparing temperature - salinity curves both from spring and from autumn, which are obtained by means of a suitable averaging process (see plate 8, 9). The resulting depths reach from less than 200 m in the southern part of the area to more than 600 m west of Scotland and south of Iceland (see plate 10, fig. 20). The mean error of these depths was found to be about 15%, The weak haline stratification in the area southeast of Greenland gives rise to the sinking of cooled surface water in winter. Therefore extreme depths of more than 2000 m may be reached by annual surface disturbances (see plate 11). This area is well known as one of the sources of North Atlantic deep water. By means of strong simplifications vertical exchange coefficients were estimated (see table 2 and 3).
    Type: Article , NonPeerReviewed
    Format: text
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