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  • Elsevier  (11)
  • Pergamon Press  (2)
  • 2015-2019  (5)
  • 1990-1994  (8)
  • 11
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    Elsevier
    In:  Earth and Planetary Science Letters, 113 (1-2). pp. 287-292.
    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
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  • 12
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    Elsevier
    In:  In: Encyclopedia of Ocean Sciences. , ed. by Cochran, J. K., Bokuniewicz, J. H. and Yager, L. P. Elsevier, Oxford, UK, pp. 189-203.
    Publication Date: 2020-12-16
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 13
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    Pergamon Press
    In:  Deep Sea Research Part A: Oceanographic Research Papers, 37 (12). pp. 1805-1823.
    Publication Date: 2020-08-04
    Description: Two stacked outflow cores of the Mediterranean Water undercurrent pass through a broad “gateway” between Cape St. Vincent and Gettysburg Bank entering the Iberian Basin. The upper core (depth ∼750 m, σ1=31.85) shows a strong tendency to follow the contours of the Portuguese continental rise. Yet, the lower core (depth ∼1250 m, σ1=32.25) primarily meanders west and northwestward forming large blobs of Mediterranean Water. The predominance of isolated Meddy structures embedded in a background field is reflected in a long-term current meter record from the deep Iberian Basin.
    Type: Article , PeerReviewed
    Format: text
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