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  • 1
    Electronic Resource
    Electronic Resource
    Grußwort (1993)
    Springer
    Ocean dynamics 45 (1993), S. 13-14 
    Details
    ISSN: 1616-7228
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02226369
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    Paper (German National Licenses)
    Fulltext
  • 2
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    First resolution of flow through the Hunter Channel in the South Atlantic (1992)
    Elsevier
    In:  Earth and Planetary Science Letters, 113 (1-2). pp. 287-292.
    Details
    Publication Date: 2018-03-02
    Description: Dense Antarctic Bottom Water formed around the continent of Antarctica spreads northward in the Atlantic underneath North Atlantic Deep Water, gradually mixing and upwelling into it. This Antarctic Water forms a significant element of the meridional circulation in both directions: northward as bottom water and southward as deep water. It is important to determine the strength of each component to assess its role in ocean circulation. Such measurements are useful when made in constricted pathways because any flow is more clearly defined. A new set of fine-resolution hydrograhic measurements in the Hunter Channel of the South Atlantic Ocean has been obtained, which allow the geostrophic bottom flow there to be estimated for the first time. The northward flow through the Hunter Channel of water cooler than 2-degrees-C is thus estimated to be 0.7 X 10(6) m3 s-1.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/0012-821X(92)90226-L
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 3
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    Consistency Relations for Internal Waves (1976)
    Elsevier
    In:  Deep Sea Research and Oceanographic Abstracts, 23 (7). pp. 613-628.
    Details
    Publication Date: 2018-03-08
    Description: A complete set of linearly independent relationships among the different cross spectral components obtained from pairs of moored instruments is derived which can be utilized to test whether or not the observed fluctuations within the internal wave frequency band represent a field of propagating internal waves. A further complete set of relationships is derived which enables to test whether or not the internal wave field is horizontally isotropic and (or) vertically symmetric. These relations are compared with corresponding relations for alternative models (standing internal wave modes, three-dimensional isotropic turbulence) and their capability to discriminate between the various models is investigated. The tests are applied to a set of data for which it is found that the observed fluctuations are consistent with both propagating and standing internal waves whereas isotropic turbulence must be rejected for the most part of the internal wave frequency band.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/0011-7471(76)90004-8,
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    OceanRep: Article in a Scientific Journal - peer-reviewed
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