INSTABILITY PROPERTIES OF ATMOSPHERIC DISTURBANCES

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    摘要 Therearesomebasicproblemsinprevioustheoreticalstudiesofbaroclinicinstability.Thederivedcriticalbaroclinitywasconsiderablylowerthanthetimeaveragedmeanmeridionaltemperaturegradient,especiallyinthelowertroposphere.Also,thelinearmechanismofbaroclinicdisturbancedevelopmentwhichisnotedrestrictedbythecriticalbaroclinitywasnotstudiedsufficiently.Therealisticcriticalbaroclinityanddisturbancedevelopmentarediscussedinthisstudy.Itwillbeshownthatthecriticalconditionofinstabilityandtypicaltimeandspacescalesofdisturbancesde-pendonthree-dimensionalstructuresofatmosphereandsphericityoftheearth,otherthanthehorizontaltemperaturegradientalone.Thevariantbehaviourofatmosphericdisturbancesdependshighlyontheirspecificscalesthatmaybedescribedbythesametheoreticalmodel.Thus,therewouldbenosubstantialdifferencesinthebasicinstabilitymecha-nismofmanydisturbancesincludingthepolarlowsandexplosivecyclones.
    作者 Yong.L.McHall
    机构地区 不详
    出处 《气象学报:英文版》 1992年2期
    出版日期 1992年02月12日(中国Betway体育网页登陆平台首次上网日期,不代表论文的发表时间)
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