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    Spatial and Temporal Variations in Antarctic Sea-Ice (1973–82)

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 003::page 470
    Author:
    Ropelewski, Chester F.
    DOI: 10.1175/1520-0450(1983)022<0470:SATVIA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Monthly estimates of Antarctic sea-ice area for the past decade were extracted from operational churts. Empirical orthogonal function analyses of these satellite-derived data revealed the existence of six distinct ice area sub-regions. Comparison of ice area time series for these sub-regions highlights the substantial differences among them. For example, total sea-ice extent typically reached a maximum in either August or September, while the Ron Sea often exhibited two relative maxima (July and October). The data show considerable year-to-year variability during this short period of record with the minimum sea-ice area varying by more than a factor of two and maximum sea-ice area varying by almost 20%. The large year-to-year variability precludes a reliable identification of longer term trends during the relatively short era of satellite observations.
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      Spatial and Temporal Variations in Antarctic Sea-Ice (1973–82)

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145583
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    contributor authorRopelewski, Chester F.
    date accessioned2017-06-09T13:59:23Z
    date available2017-06-09T13:59:23Z
    date copyright1983/03/01
    date issued1983
    identifier issn0733-3021
    identifier otherams-10463.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145583
    description abstractMonthly estimates of Antarctic sea-ice area for the past decade were extracted from operational churts. Empirical orthogonal function analyses of these satellite-derived data revealed the existence of six distinct ice area sub-regions. Comparison of ice area time series for these sub-regions highlights the substantial differences among them. For example, total sea-ice extent typically reached a maximum in either August or September, while the Ron Sea often exhibited two relative maxima (July and October). The data show considerable year-to-year variability during this short period of record with the minimum sea-ice area varying by more than a factor of two and maximum sea-ice area varying by almost 20%. The large year-to-year variability precludes a reliable identification of longer term trends during the relatively short era of satellite observations.
    publisherAmerican Meteorological Society
    titleSpatial and Temporal Variations in Antarctic Sea-Ice (1973–82)
    typeJournal Paper
    journal volume22
    journal issue3
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1983)022<0470:SATVIA>2.0.CO;2
    journal fristpage470
    journal lastpage473
    treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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