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    Length-of-Day Changes and Mountain Torque during El Nifio

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 024::page 3656
    Author:
    Wolf, Wendy L.
    ,
    Smith, Ronald B.
    DOI: 10.1175/1520-0469(1987)044<3656:LODCAM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Values of mountain pressure torque are calculated for the Rocky and Andes Mountains and for the Tibetan Plateau in order to evaluate their conuibufion to the observed anomalous length-of-day (LOD) and atmospheric angular momentum (AAM) change during the period from late January to mid-February 1983. A period of rapid increase in AAM and LOD is found to coincide with unusually high values of mountain torque on the Rocky Mountains, associated with a midcontinent high-pressure event and a sequence of Pacific frontal cyclone lows hitting California. A subsequent decrease in AAM is not correlated with mountain pressure torquesover the three regions tested, thus implicating other regions or other transfer mechanisms.
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      Length-of-Day Changes and Mountain Torque during El Nifio

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4155846
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    contributor authorWolf, Wendy L.
    contributor authorSmith, Ronald B.
    date accessioned2017-06-09T14:27:50Z
    date available2017-06-09T14:27:50Z
    date copyright1987/12/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19700.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155846
    description abstractValues of mountain pressure torque are calculated for the Rocky and Andes Mountains and for the Tibetan Plateau in order to evaluate their conuibufion to the observed anomalous length-of-day (LOD) and atmospheric angular momentum (AAM) change during the period from late January to mid-February 1983. A period of rapid increase in AAM and LOD is found to coincide with unusually high values of mountain torque on the Rocky Mountains, associated with a midcontinent high-pressure event and a sequence of Pacific frontal cyclone lows hitting California. A subsequent decrease in AAM is not correlated with mountain pressure torquesover the three regions tested, thus implicating other regions or other transfer mechanisms.
    publisherAmerican Meteorological Society
    titleLength-of-Day Changes and Mountain Torque during El Nifio
    typeJournal Paper
    journal volume44
    journal issue24
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<3656:LODCAM>2.0.CO;2
    journal fristpage3656
    journal lastpage3660
    treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 024
    contenttypeFulltext
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