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G%W|rFV W|tw;Tu;D rt PDXeldclassificatirdingtothefrequencyofcloudbaseheightoccurenceMegicalForecasts,L.,1985,8590.AtechniqueforcloudfassificationisgivendevelopedonthebasisofKintragrrages.Howeverunlikethisalgorithm,classcentresarecromtheconditionoftheirmostuniformpositioningondscaleandthenumberofclassesisnotpreset.AcriterofferedforselectingoptimumclassificationofcloudfieordingtothefrequencyofoccurenceofcloudbaseforApWesternEurope. XXX XhenkoP.Ye.,andB.Kh.Thamokov.1986.TheeffectofmictureontheDopplerradarcharacteristicsofhailclouds.edingsofHighMountainGeophysicalInstitute.63:10111inctionandreflectancecoefficients,averagegravitationty,rootmeansquarewidthsofgravitationvelocityspectthsfortwophaserainhailmixturearecalculated.Hailumedtobemeltingwith h =0.01cm.Calculationswefor 0*%0 differentversionsofrainhaildistributionfunctionfor=3.2cm.Itisshownthatrmaldistributioninthecaseof P-(4 rainotdescribethewholerangeofvelocitiesobserved.Thesionismadeonthenecessityoftakingintoaccounttheeofrainhailmixtureinhailcloudsintheoreticalcalcs.MartinesD.,K.Peres,V.P.Belyayev,andVov.1989.Thermodynamiccharacteristicsoftropicalconvelouds.TropicalMeteorology:Proc.,FourthInternationalium,Havana,1317Apr.1987,Leningrad.pp.351360.Oredandtwoconvectivecloudsfrom0.4to10kmthickweinedwiththehelpofaircraftonboardinstruments,thatsureverticalmotionsandtemperaturepulsations.Informasobtainedonthethermodynamiccharacteristicsofthewtsofconvectiveclouds.Itisshownthatamplitudesoferisticsincloudsincreasewiththeincreaseintheirth.Verticalvelocitiesinthickcumuluscloudsamountedt18.0m/sec1andtemperaturedisturbancesfrom2.5$  $ C.Severalupdrafts,afewhuetersstrongwereobservedalternatingwithdowndrafts.tivelysmallcumuluscloudscommonlyhaveonlyoneupdrafem100300minsize.L.T.Matveyev.19studyingclouddynamics.Interinst.CollectionofLeningromet.Inst.73:3145. P-(4 Areviewofpathedynamicsofclouds,whichwasstartedintheSovietboutfiveyearsago.BasicresultsandideasunderlyingRQ&4X[;u.;t2(X[;u*;t$҃& u3ɋ&3&X[ t tX[ u&X[RZ&X[RZĀt;r/ƀtu ) &X[1ș&X[&ȋ&X[ȋ&X[ȋ&X[##&X[3X[ &[P=bXtPSQbؠ 6tY[XWV[PPSQbؠ 6tY[XW*[P=bXtPSQbؠ