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  • 1990-1994  (3)
Document type
Publisher
Years
Year
  • 1
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    Unknown
    On the formation and spreading of the Bass Strait cascade (1994)
    Elsevier
    In:  Continental Shelf Research, 14 (4). pp. 385-399.
    Details
    Publication Date: 2018-08-17
    Description: The Bass Strait cascade is a wintertime downwelling caused by cooling of the shallow waters of Bass Strait. During winter, a front separates the cold shelf water from the waters of the Tasman Sea. Continuous horizontal bands of downwelled water leading oceanward beneath the front imply that it can be transgressed near the bottom anywhere along its length. However, by far the greatest volume crosses at a breach at the northern end. Measured currents in eastern Bass Strait fit a predictable pattern: eastward toward the front, then as the front is approached, swinging north towards the breach. Flow northwards along the slope after downwelling is quantified using a simple analytic model. Cascade water found in the “far-field” was found only in small patches. One such patch was found to possess motion independent from the mean flow in which it was embedded.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/0278-4343(94)90025-6
    Location Call Number Limitation Availability
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 2
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    Unknown
    The Mediterranean water tongue and its chlorofluoromethane signal in the Iberian Basin in early summer 1989 (1993)
    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research: Oceans, 98 (C5). p. 8405.
    Details
    Publication Date: 2019-09-23
    Description: Hydrographic observations from the Iberian Basin demonstrate the variability of water masses in upper and intermediate layers. The surveyed area embraces the internal front between water masses from higher latitudes and the Mediterranean outflow, exhibits several isolated Mediterranean eddy (meddy) structures at middepth, and displays the virtual source region for the Mediterranean Water (MW) tongue off the Portuguese continental slope. The description is enhanced by additional chlorofluoromethane measurements, which show anomalously high concentrations at middepth, due to mixing of MW with the overlying Atlantic waters in the Gulf of Cadiz. The geostrophic stream function shows several meddylike features that not only are remarkably extended in the depth range of the MW, but are also correlated with surface height anomalies.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1029/93JC00040
    Location Call Number Limitation Availability
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 3
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    Unknown
    Meddies - Wirbel aus Mittelmeerwasser im Ostatlantik (1993)
    Spektrum d. Wiss. Verl.-Ges.
    In:  Spektrum der Wissenschaft, 11 . pp. 29-34.
    Details
    Publication Date: 2016-06-20
    Description: Salzreiches Wasser, das durch die Straße von Gibraltar aus dem Mittelmeer in den Atlantik strömt, wird dort verwirbelt und driftet teilweise als rotierende Salzlinse in etwa 1000 Meter Tiefe manchmal mehr als zwei Jahre lang bis zu 1000 Kilometer weit, ehe es sich endgültig mit dem Atlantikwasser vermischt.
    Type: Article , NonPeerReviewed
    Location Call Number Limitation Availability
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    OceanRep: Article in a Scientific Journal - without review
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