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    Precipitation Signatures in Sea-Surface-Layer Conditions During BOMEX

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003::page 498
    Author:
    Elliott, Garry W.
    DOI: 10.1175/1520-0485(1974)004<0498:PSISSL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Observations were made during the Barbados Oceanographic and Meteorological Experiment in 1969 to evaluate the possibility of determining total precipitation from the change in salinity or temperature at the ocean surface. Salinity-temperature-depth soundings were taken at 3-hr intervals during periods of no rain, and at 5- to 6-min intervals during periods of rain. Analysis of salinity data shows that during periods of no rain, salinity regularly fluctuated by ±0.15?. Fluctuations of this magnitude are likely to obscure possible salinity depressions due to rainfall. No rainfall-related, long-term depressions of salinity depressions were evident. However, many sharp, short-term depressions of salinity, with duration on the order of 10 to 45 min, were observed during periods of rainfall.
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      Precipitation Signatures in Sea-Surface-Layer Conditions During BOMEX

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4162241
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    contributor authorElliott, Garry W.
    date accessioned2017-06-09T14:43:57Z
    date available2017-06-09T14:43:57Z
    date copyright1974/07/01
    date issued1974
    identifier issn0022-3670
    identifier otherams-25456.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162241
    description abstractObservations were made during the Barbados Oceanographic and Meteorological Experiment in 1969 to evaluate the possibility of determining total precipitation from the change in salinity or temperature at the ocean surface. Salinity-temperature-depth soundings were taken at 3-hr intervals during periods of no rain, and at 5- to 6-min intervals during periods of rain. Analysis of salinity data shows that during periods of no rain, salinity regularly fluctuated by ±0.15?. Fluctuations of this magnitude are likely to obscure possible salinity depressions due to rainfall. No rainfall-related, long-term depressions of salinity depressions were evident. However, many sharp, short-term depressions of salinity, with duration on the order of 10 to 45 min, were observed during periods of rainfall.
    publisherAmerican Meteorological Society
    titlePrecipitation Signatures in Sea-Surface-Layer Conditions During BOMEX
    typeJournal Paper
    journal volume4
    journal issue3
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1974)004<0498:PSISSL>2.0.CO;2
    journal fristpage498
    journal lastpage501
    treeJournal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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