摘要
Therearesomebasicproblemsinprevioustheoreticalstudiesofbaroclinicinstability.Thederivedcriticalbaroclinitywasconsiderablylowerthanthetimeaveragedmeanmeridionaltemperaturegradient,especiallyinthelowertroposphere.Also,thelinearmechanismofbaroclinicdisturbancedevelopmentwhichisnotedrestrictedbythecriticalbaroclinitywasnotstudiedsufficiently.Therealisticcriticalbaroclinityanddisturbancedevelopmentarediscussedinthisstudy.Itwillbeshownthatthecriticalconditionofinstabilityandtypicaltimeandspacescalesofdisturbancesde-pendonthree-dimensionalstructuresofatmosphereandsphericityoftheearth,otherthanthehorizontaltemperaturegradientalone.Thevariantbehaviourofatmosphericdisturbancesdependshighlyontheirspecificscalesthatmaybedescribedbythesametheoreticalmodel.Thus,therewouldbenosubstantialdifferencesinthebasicinstabilitymecha-nismofmanydisturbancesincludingthepolarlowsandexplosivecyclones.
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)