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  • Other Sources  (6)
  • NORSAR  (4)
  • Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research
  • American Institute of Physics (AIP)
  • Nature Publishing Group
  • 2005-2009
  • 1985-1989  (6)
  • 1950-1954
  • 1986  (6)
  • 1
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    NORSAR
    In:  Semiannual technical summary, April - September 1986, NORSAR scientific report, Oslo, NORSAR, vol. C 560, 183 pp., no. 1-86/87, pp. 1058-1061, (ISBN 3-933346-037)
    Publication Date: 1986
    Keywords: Seismic arrays ; Data analysis / ~ processing ; Seismology ; f-k-Analysis
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  • 2
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    NORSAR
    In:  NORESS Research Symposium, Houston, NORSAR, vol. C 560, 183 pp., no. 1254, pp. 160-168, (ISBN 3-933346-037)
    Publication Date: 1986
    Keywords: Data analysis / ~ processing ; Expert systems ; Seismology ; Seismic arrays
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  • 3
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    NORSAR
    In:  Semiannual technical summary, October 1985 - March 1986, NORSAR Scientific Report, Oslo, NORSAR, vol. C 560, 183 pp., no. 2-85/86, pp. 1058-1061, (ISBN 3-933346-037)
    Publication Date: 1986
    Description: Anwendung der Drei-Komponenten-Analyse auf regionale Seismogramme von NORSAR. Mehrere Drei-Komponenten-Sensoren in einer Array-Konfiguration. Partikel-Bewegung wurde bestimmt aus der Kovarianz im Frequ.bereich, Erweiterung des Algorithmus durch Benutzung des Maximum-Likelihood-Prinzips. Neben erfolgreicher Bestimmung vom Azimut fanden sie, daß 3-Komp.-Information nützlich ist zur Detektion sekundärer Phasen Sn und Lg und zeigen Vorschläge zur Unterscheidung beider auf.
    Keywords: Seismology ; Polarization ; Seismic arrays ; Three component data
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  • 4
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    NORSAR
    In:  Contribution, Arlington, Virgina, NORSAR, vol. 10, no. 366, pp. 30
    Publication Date: 1986
    Keywords: Polarization
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  • 5
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    Nature Publishing Group
    In:  Nature, 320 (6058). pp. 107-108.
    Publication Date: 2016-03-01
    Type: Article , PeerReviewed
    Format: text
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  • 6
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    Nature Publishing Group
    In:  Nature, 319 . pp. 574-576.
    Publication Date: 2019-01-21
    Description: One of the most striking features of the upper North Atlantic Ocean is an extensive layer of water with temperature close to 18°C and salinity close to 36.5‰, (ref. 1). This 18°C water is formed by winter convection in the Sargasso sea2,3, but aspects of the annual rate of 18°C water formation remain obscure4. We have simulated this water mass formation by integrating a one-dimensional model along a 4-yr trajectory of a water column circulating around the Sargasso Sea. Winter convection is deep (≥200 m) in regions where the ocean suffers a net annual heat loss to the atmosphere, and shallow (≤lOOm) where the ocean gains heat each year. The origin of the thermostad (nearly isothermal layer) is a thick layer of nearly homogeneous water subducted beneath the seasonal boundary layer in the year that the water column passes through the line dividing annual cooling from annual heating. We estimate the annual production of 18°C water to be 446,000 km3 yr−1. Downstream, more stratified central water is formed each year at a rate that depends more on Ekman pumping (wind-forced convergence) than on the decreasing depth of winter convection
    Type: Article , PeerReviewed
    Format: text
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