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  • AGU (American Geophysical Union)  (1)
  • Kiel : Inst. für Meereskunde, Abt. Physikalische Ozeanographie  (1)
  • 1995-1999  (2)
  • 1
    Book
    Book
    Kiel : Inst. für Meereskunde, Abt. Physikalische Ozeanographie
    Keywords: Report ; Kanarenbecken ; Expedition ; Poseidon ; Geschichte 1994-1998
    Description / Table of Contents: Im Rahmen der ESTOC (European Station for Time Series in the Ocean, Canary Islands) und CANIGO (Canary Islands Azores Gibraltar Observations) Projekte fanden mehrere Expeditionen mit FS Poseidon und FS Meteor im östlichen Kanarenbecken statt. Die ESTOC / CANGIO Fahren von FS Poseidon beinhalten die Reisen 202/1 im September - Oktober 1994, Reise 212 im September - Oktober 1995, Reise 233 im September - Oktober 1997 und die Reise 237/3 im April 1998. Die Fahrtberichte dieser vier von FS Poseidon Reisen werden hier durch die Fahrtleiter zusammengefasst. Beiträge anderer Fahrtteilnehmer sind als solche gekennzeichnet.
    Type of Medium: Book
    Pages: 78 S , graph. Darst., Kt , 30 cm
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 302
    Language: English
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  • 2
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    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research: Oceans, 103 (C3). pp. 5429-5437.
    Publication Date: 2018-04-17
    Description: Current measurements from three moored arrays on the Brazilian continental slope between 20 degrees S and 28 degrees S are investigated for the existence and strength of western boundary currents from near the surface down to the North Atlantic Deep Water. The Brazil Current is found to deepen southward from 100 m to more than 670 m and to strengthen its volume transport to 16.2 x 10(6) m(3)/s. Antarctic Intermediate Water is transported in a well-developed boundary current southward at 28 degrees S and northward north of Cabo Frio (24 degrees S). This result supports earlier suggestions derived from the analysis of hydrographic data that Antarctic Intermediate Water enters the Brazil Basin from the east and bifurcates as it meets the continental break off Brazil. North Atlantic Deep Water is transported southward in a weakly developed boundary current that leads to lower estimates of volume transport than expected from earlier hydrographic data analysis.
    Type: Article , PeerReviewed
    Format: text
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