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OUTLINE 1. Nucleation of water droplets (6.1) 2. Microstructures of warm clouds (6.2) 3. Cloud Liquid Water Content and Entrainment (6.3) 4. Growth of Water Droplets and Formation of Rain (6.4) 5. Microphysics of Ice Clouds (6.5) 6. Cloud Names, Lightning and Chemistry (6.7) Microphysics of Ice Clouds Cloudsbelowthe0˚isothermare referredtoaswarmclouds. Cloudsabovearecalledcoldclouds. Microphysics of Ice Clouds Microphysics of Ice Clouds Microphysics of Ice Clouds Microphysics of Ice Clouds water WHATARESUPERCOOLEDDROPLETS? -Liquidwaterthatexistsincloudsattemperaturesbelow0˚C HOMOGENEOUSNUCLEATIONOFICEPARTICLES - ChangeaggregaOonoffrozenwaterleadingtothegrowthofan icecloudparOcle.Onlywaterispresent. IcenucleaOonprocesses: CondensaOon-Freezing:2stepprocess,watervaporcondensesto formaliquid,thentheliquidfreeze. DeposiOon:transferofwatervapordirectlytoice *WewillnotcoverpreacOvaOoninthisclass.Skipfigure6.30. SaturaOonwithrespecttoliquidvsice FocusonBlueCurve. Usey-axisontherighthandside. Takehomemessage: es>esi SecOon6.5.4:FormaOonofprecipitaOonincoldclouds Cold-rainprocess(Wegener-Bergeron-FindeisenProcess SupercooledvapordropletsaccumulateonaniceparOclethroughdeposiOon oppositeofsublimaOon. subsaturatedenvironmentforliquidwaterbutasupersaturatedenvironmentforice. AlternatetodeposiOonalgrowth? RimingandaggregaOon(growthrateincreaseswithsize) RADARECHOTOMEASURECLOUDMICROPHYSICS LargeiceparOclesgrow,fall,andmelttoformrain. OUTLINE 1. Nucleation of water droplets (6.1) 2. Microstructures of warm clouds (6.2) 3. Cloud Liquid Water Content and Entrainment (6.3) 4. Growth of Water Droplets and Formation of Rain (6.4) 5. Microphysics of Ice Clouds (6.5) 6. Cloud Names, Lightning and Chemistry (6.7) LIGHTNING! - Allcloudsallelectrifiedto somedegree - InvigorousconvecOve clouds,sufficientelectrical chargesareseparatedto produceelectricfieldsthat exceedthedielectric breakdownofcloudyair, resulOnginaniniOal intraclouddischarge. - ExactmechanismissOll debated.Butclearly, rimersplayarole. RIMER:graupelorhailstone. GRAUPEL:snowcrystalcoated byriming. LIGHTNING! Achargemovesup fromthegroundto meetthecharge originaOnginthe cloud. LIGHTNING! Inclassexercise Separateintogroupsof4 PhaseI:Rapidresponseround (1minute) Listinbulletpointsthelifecycleofwatervaporinanairparcelthatendsasrain ontheground. PhaseII:Keyfigures (5minutes) SketchthekeyfiguresfromtheMicrophysicschapter(labeltheaxes). PhaseIII:Relaxedresponseround (5minutes) Listinbulletpointsthelifecycleofwatervaporinanairparcelthatendsasrain ontheground.IncludeesOmatesforthesizeoftheliquidparOcle. CLOUDANDPRECIPITATION PROCESSESTHATAFFECT ATMOSPHERICCHEMISTRY