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    The Characteristic Spatial and Temporal Scales for SLP, SST, and Air Temperature in the Southern Hemisphere

    Source: Journal of Applied Meteorology:;1990:;volume( 029 ):;issue: 008::page 694
    Author:
    Colosi, John
    ,
    Barnett, Tim P.
    DOI: 10.1175/1520-0450(1990)029<0694:TCSATS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This study summarizes results of an analysis of the TOGA drifting buoy observations in the Southern Hemisphere. The data were first quality controlled for gross errors and then screened against climatology and products from national weather centers. The characteristic space scales of the SLP, SST, and air temperature fields for the summer months of December, January, and February, and the winter months of June, July, and August were determined next. Typical decorrelation distances for all fields were between 1200?2800 km with the correlations being generally isotropic. This information suggests that roughly 30?40 fully functional buoys evenly distributed over the southern oceans from 15° to 60°S should be able to resolve the major scales of Southern Hemisphere climate change.
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      The Characteristic Spatial and Temporal Scales for SLP, SST, and Air Temperature in the Southern Hemisphere

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146826
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    contributor authorColosi, John
    contributor authorBarnett, Tim P.
    date accessioned2017-06-09T14:03:09Z
    date available2017-06-09T14:03:09Z
    date copyright1990/08/01
    date issued1990
    identifier issn0894-8763
    identifier otherams-11582.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146826
    description abstractThis study summarizes results of an analysis of the TOGA drifting buoy observations in the Southern Hemisphere. The data were first quality controlled for gross errors and then screened against climatology and products from national weather centers. The characteristic space scales of the SLP, SST, and air temperature fields for the summer months of December, January, and February, and the winter months of June, July, and August were determined next. Typical decorrelation distances for all fields were between 1200?2800 km with the correlations being generally isotropic. This information suggests that roughly 30?40 fully functional buoys evenly distributed over the southern oceans from 15° to 60°S should be able to resolve the major scales of Southern Hemisphere climate change.
    publisherAmerican Meteorological Society
    titleThe Characteristic Spatial and Temporal Scales for SLP, SST, and Air Temperature in the Southern Hemisphere
    typeJournal Paper
    journal volume29
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1990)029<0694:TCSATS>2.0.CO;2
    journal fristpage694
    journal lastpage703
    treeJournal of Applied Meteorology:;1990:;volume( 029 ):;issue: 008
    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
    yabeshDSpacePersian