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  • 1
    Electronic Resource
    Electronic Resource
    Satellite measurements of sea surface cooling during hurricane Gloria (1987)
    [s.l.] : Nature Publishing Group
    Nature 326 (1987), S. 373-375 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Hurricane Gloria (1985) began to form very late in the hurricane season off the Cape Verde Islands1. Gloria moved nearly due westward with the trade winds to about the Leeward Islands, and then turned north-west toward the Sargasso Sea. On 25 September the minimum central pressure fell to 919 mbar, ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/326373a0
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    Paper (German National Licenses)
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  • 2
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    Satellite measurements of sea surface cooling during hurricane Gloria (1987)
    Nature Publishing Group
    In:  Nature, 326 (6111). pp. 373-375.
    Details
    Publication Date: 2018-03-02
    Description: Hurricanes and other strong storms can cause important decreases in sea surface temperature by means of vertical mixing within the upper ocean, and by air–sea heat exchange. Here we use satellite-derived infrared images of the western North Atlantic to study sea surface cooling caused by hurricane Gloria (1985). Significant regional variations in sea surface cooling are well correlated with hydrographic conditions. The greatest cooling (up to 5°C) occurred in slope waters north of the Gulf Stream where the seasonal thermocline is shallowest and most compressed; moderate cooling (up to 3 °C) occurred in the open Sargasso Sea where the thermocline is deeper and more diffused; little or no cooling occurred in shallow coastal waters (bottom depth less than 20 m) which were isothermal before the passage of hurricane Gloria. There is a pronounced right-side asymmetry of sea surface cooling with stronger (by a factor of 4) and more extensive (by a factor of 3) cooling found on the right side of the hurricane track. These qualitative results are consistent with the notion that vertical mixing within the upper ocean is the dominant sea surface cooling mechanism of hurricanes.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
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