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    Further Evidence of Traveling Planetary Waves

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 009::page 1605
    Author:
    Madden, Roland A.
    DOI: 10.1175/1520-0469(1978)035<1605:FEOTPW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Evidence of regularly propagating, large-scale waves is found in a 73-year record of Northern Hemisphere sea-level pressure data and in a nine-year record of upper air data. Cross-spectrum analyses indicate that south of 50°N, in all seasons, a zonal wavenumber 1 disturbance moves westward around the world in 5 days. In addition, north of 50°N a zonal wavenumber 1 disturbance moves westward around the world in one to three weeks with an average period near 16 days. This disturbance appears to be strongest in winter and spring. The structure of the 16-day wave during winter is studied in detail, and it is shown to be consistent, in many respects, with that of a theoretically predicted free planetary wave, or wave of the second class. A similar conclusion can be made concerning the 5-day wave.
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      Further Evidence of Traveling Planetary Waves

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153448
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    contributor authorMadden, Roland A.
    date accessioned2017-06-09T14:20:18Z
    date available2017-06-09T14:20:18Z
    date copyright1978/09/01
    date issued1978
    identifier issn0022-4928
    identifier otherams-17542.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153448
    description abstractEvidence of regularly propagating, large-scale waves is found in a 73-year record of Northern Hemisphere sea-level pressure data and in a nine-year record of upper air data. Cross-spectrum analyses indicate that south of 50°N, in all seasons, a zonal wavenumber 1 disturbance moves westward around the world in 5 days. In addition, north of 50°N a zonal wavenumber 1 disturbance moves westward around the world in one to three weeks with an average period near 16 days. This disturbance appears to be strongest in winter and spring. The structure of the 16-day wave during winter is studied in detail, and it is shown to be consistent, in many respects, with that of a theoretically predicted free planetary wave, or wave of the second class. A similar conclusion can be made concerning the 5-day wave.
    publisherAmerican Meteorological Society
    titleFurther Evidence of Traveling Planetary Waves
    typeJournal Paper
    journal volume35
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1978)035<1605:FEOTPW>2.0.CO;2
    journal fristpage1605
    journal lastpage1618
    treeJournal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 009
    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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