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  • Institut für Meereskunde  (5)
  • Nature Publishing Group  (2)
  • 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: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Ocean temperature, salinity and chlorofluorocarbon concentration data are used to track the recent spreading of cold intermediate-depth water masses from the Labrador Sea across the northern North Atlantic Ocean. These water masses, which are formed from surface waters by deep convection in ...
    Type of Medium: Electronic Resource
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  • 3
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    Nature Publishing Group
    In:  Nature, 397 . pp. 243-246.
    Publication Date: 2017-02-28
    Description: The overflow and descent of cold dense water from the Denmark Strait sill-a submarine passage between Greenland and Iceland-is a principal means by which the deep ocean is ventilated, and is an important element in the global thermohaline circulation. Previous investigations of its variability-in particular, direct current measurements(1,2) in the overflow core since 1986-have shown surprisingly little evidence of long-term changes in now speed. Here we report significant changes in the overflow characteristics during the winter of 1996-97, measured using two current-meter moorings and an inverted echo sounder located at different depths in the fastest part of the now. The overflow warmed to the highest monthly value yet recorded (2.4 degrees C), and showed a pronounced slowing and thinning at its lower margin. We believe that the extreme warmth of the overflow caused it to run higher on the continental slope off east Greenland, so that the lower current meters and the echo sounder were temporarily outside and deeper than the fast-flowing core; model simulations appear to confirm this interpretation, We suggest that the extreme warmth of the overflow is a lagged response to a warming upstream in the Fram Strait three years earlier (caused by an exceptional amplification of the winter North Atlantic Oscillation). If this is so, over-now characteristics may be predictable.
    Type: Article , PeerReviewed
    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, 119 . Institut für Meereskunde, Kiel, Germany, 68 pp.
    Publication Date: 2016-09-08
    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, 134 . Institut für Meereskunde, Kiel, Germany, 60 pp.
    Publication Date: 2014-12-12
    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, 146 . Institut für Meereskunde, Kiel, Germany, 80 pp.
    Publication Date: 2019-09-23
    Type: Report , NonPeerReviewed
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  • 7
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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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  • 8
    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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