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Cloud Dynamics, Volume 104, Second Edition PDF

457 Pages·2014·45.316 MB·English
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International Geophysics Volume 104 Cloud Dynamics Second Edition This page intentionally left blank International Geophysics Volume 104 Cloud Dynamics Second Edition Robert A. Houze, Jr. Department of Atmospheric Sciences University of Washington Seattle, Washington AMSTERDAM (cid:129) BOSTON (cid:129) HEIDELBERG (cid:129) LONDON NEW YORK (cid:129) OXFORD (cid:129) PARIS (cid:129) SAN DIEGO SAN FRANCISCO (cid:129) SINGAPORE (cid:129) SYDNEY (cid:129) TOKYO Academic Press is an imprint of Elsevier AcademicPressisanimprintofElsevier TheBoulevard,LangfordLane,Kidlington,OxfordOX51GB,UK Radarweg29,POBox211,1000AEAmsterdam,TheNetherlands SecondEdition Copyright©2014ElsevierInc.Allrightsreserved. FirstEdition Copyright©1993AcademicPressInc.PublishedbyElsevierB.V.Allrightsreserved. Nopartofthispublicationmaybereproduced,storedinaretrievalsystemortransmittedinanyformorbyany meanselectronic,mechanical,photocopying,recordingorotherwisewithoutthepriorwrittenpermission ofthepublisher. PermissionsmaybesoughtdirectlyfromElsevier’sScience&TechnologyRightsDepartmentinOxford,UK: phone(+44)(0)1865843830;fax(+44)(0)1865853333;email:[email protected] youcansubmityourrequestonlinebyvisitingtheElsevierwebsiteathttp://elsevier.com/locate/permissions, andselectingObtainingpermissiontouseElseviermaterial. Notice Noresponsibilityisassumedbythepublisherforanyinjuryand/ordamagetopersonsorpropertyasamatter ofproductsliability,negligenceorotherwise,orfromanyuseoroperationofanymethods,products, instructionsorideascontainedinthematerialherein.Becauseofrapidadvancesinthemedicalsciences,in particular,independentverificationofdiagnosesanddrugdosagesshouldbemade. BritishLibraryCataloguinginPublicationData AcataloguerecordforthisbookisavailablefromtheBritishLibrary LibraryofCongressCataloging-in-PublicationData AcatalogrecordforthisbookisavailablefromtheLibraryofCongress ISBN:978-0-12-374266-7 ISSN:0074-6142 ForinformationonallAcademicPresspublications visitourwebsiteatstore.elsevier.com PrintedandboundinChina 14 15 16 17 18 10 9 8 7 6 5 4 3 2 1 Dedication To Yolanda Rebecca and Deborah Gabriel, Margaret, Lucian, Alice, and Elizabeth This page intentionally left blank Contents Dedication v 2.5. PotentialVorticity 31 Preface xiii 2.6. PerturbationFormsoftheEquations 32 ListofSymbols xv 2.6.1. AverageandPerturbationForms oftheEquationofStateand ContinuityEquation 32 2.6.2. FluxFormsandLinearization Part I oftheThermodynamicand Fundamentals Water-ContinuityEquations 32 2.6.3. FluxFormandLinearization 1. Types of Clouds in Earth’s oftheEquationofMotion 33 Atmosphere 2.6.4. EddyKineticEnergyEquation 33 3 2.7. OscillationsandWaves 33 1.1. AtmosphericStructureandScales 3 2.7.1. BuoyancyOscillations 33 1.2. CloudTypesIdentifiedVisually 4 2.7.2. GravityWaves 34 1.2.1. Genera,Species,andE´tages 4 2.7.3. InertialOscillations 35 1.2.2. LowClouds 6 2.7.4. Inertio-GravityWaves 36 2.8. AdjustmenttoGeostrophicand 1.2.3. MiddleClouds 10 1.2.4. HighClouds 12 GradientBalance 36 1.2.5. OrographicClouds 13 2.9. Instabilities 38 1.2.6. NoctilucentClouds 16 2.9.1. Buoyant,Inertial,andSymmetric 1.3. PrecipitatingCloudSystems 16 Instabilities 38 1.3.1. MesoscaleConvectiveSystems 17 2.9.2. Kelvin–HelmholtzInstability 40 1.3.2. TropicalCyclones 17 2.9.3. Rayleigh–Be´nardInstability 42 1.3.3. ExtratropicalCyclones 18 2.10. RepresentationofEddyFluxes 44 1.4. SatelliteCloudClimatology 20 2.10.1. K-Theory 44 2.10.2. HigherOrderClosure 45 2. Atmospheric Dynamics 25 2.10.3. LargeEddySimulation 45 2.11. ThePlanetaryBoundaryLayer 45 2.1. TheBasicEquations 25 2.11.1. TheEkmanLayer 45 2.1.1. EquationofMotion 25 2.11.2. Boundary-LayerStability 46 2.1.2. EquationofState 25 2.11.3. TheSurfaceLayer 46 2.1.3. ThermodynamicEquation 25 2.1.4. MassContinuity 26 3. Cloud Microphysics 47 2.1.5. WaterContinuity 26 2.1.6. TheFullSetofEquations 27 3.1. MicrophysicsofWarmClouds 47 2.2. BalancedFlow 27 3.1.1. NucleationofDrops 47 2.2.1. QuasigeostrophicMotion 27 3.1.2. CondensationandEvaporation 49 2.2.2. SemigeostrophicMotions 27 3.1.3. FallspeedsofDrops 50 2.2.3. GradientWindBalance 28 3.1.4. ContinuousCollection 51 2.2.4. HydrostaticBalance 29 3.1.5. StochasticCollection 52 2.2.5. ThermalWind 29 3.1.6. SpontaneousandCollisional 2.2.6. CyclostrophicBalance 29 BreakupofDropsandModification 2.3. AnelasticandBoussinesqapproximations 29 oftheStochasticCollection 2.4. Vorticity 31 Formulation 53 vii viii Contents 3.2. MicrophysicsofColdClouds 54 4.7. EstimatingArealPrecipitation 3.2.1. HomogeneousNucleation fromRadarData 88 ofIceParticles 54 4.8. DeterminingCloudMorphology 3.2.2. HeterogeneousNucleation fromRadarData 89 andOtherProcessesFormingSmall 4.9. DopplerRadar 89 IceParticlesinClouds 55 4.9.1. RadialVelocity 90 3.2.3. VaporDepositionandSublimation 57 4.9.2. VelocityandRangeFolding 91 3.2.4. AggregationandRiming 58 4.9.3. VerticalIncidenceObservations 91 3.2.5. Hail 60 4.9.4. Range-HeightData 92 3.2.6. IceEnhancement 61 4.9.5. Velocity-AzimuthDisplayMethod 92 3.2.7. FallspeedsofIceParticles 62 4.9.6. MultipleDopplerSynthesis 94 3.2.8. Melting 64 4.9.7. RetrievalofThermodynamicand 3.3. TypesofMicrophysicalProcessesand MicrophysicalVariables 95 CategoriesofWaterSubstanceinClouds 65 3.4. Water-ContinuityEquations 67 Part II 3.5. BinWater-ContinuityModels 68 3.5.1. General 68 Phenomena 3.5.2. BinModelingofWarmClouds 68 3.5.3. BinModelingofColdClouds 69 5. Clouds in Shallow Layers at Low, 3.6. BulkWater-ContinuityModels 70 Middle, and High Levels 101 3.6.1. TheClassicKesslerApproachtoBulk Water-ContinuityModelingofWarm 5.1. FogandStratusOccurringinaBoundary PrecipitatingClouds 70 LayerCooledfromBelow 101 3.6.2. MultimomentBulkWater-Continuity 5.1.1. GeneralConsiderations 101 ModelingofWarmClouds 72 5.1.2. TurbulentMixinginFog 102 3.6.3. BulkModelingofColdCloudsBy 5.1.3. RadiationFog 104 ExtendingtheKesslerScheme 74 5.1.4. ArcticStratusandStratocumulus 108 3.7. Water-ContinuityModelingofCold 5.2. StratocumulusForminginBoundary CloudsUsingGeneralizedMass-Size LayersHeatedfromBelow 111 andArea-SizeRelations 75 5.2.1. Climatology 111 5.2.2. ConceptualModeloftheFormation 4. Remote Sensing of Clouds and ofaCloudToppedMixedLayer 112 Precipitation 77 5.2.3. MathematicalModelingof CloudToppedMixedLayer 4.1. Absorption,Scattering,andthe Formation 114 MicrowaveDomain 78 5.2.4. StratocumuluswithDrizzle 118 4.2. PassiveMicrowaveSensingof 5.2.5. LaterStagesoftheStratocumulus Precipitation 79 Lifecycle 118 4.3. RadarSensingofCloudsand 5.2.6. CellularStructuresandPatternsin Precipitation 80 StratocumulusFields 118 4.4. RadarReflectivityfromReturnedPower 82 5.2.7. BoundaryLayerRollsandCloud 4.5. RadarPolarimetry 84 Streets 120 4.5.1. ParametersMeasuredby 5.3. AltostratusandAltocumulus 124 Dual-PolarizationRadar 84 5.3.1. AltostratusandAltocumulus 4.5.2. IdentificationofHydrometeor ProducedasRemnantsofOther TypewithDual-PolarizationRadar 85 Clouds 124 4.6. RelatingRadarMeasurementsto 5.3.2. AltocumulusasHighBased HydrometeorConcentration, ConvectiveClouds 125 Precipitation,FallVelocity,and 5.3.3. AltostratusandAltocumulus Cloud-SystemStructure 86 asShallowLayerCloudsAloft 125 4.6.1. Particle-SizeMethod 86 5.3.4. IceParticleGenerationBy 4.6.2. Rain-GaugeMethod 87 AltocumulusElements 127 4.6.3. PolarimetricImprovementofRain 5.3.5. InteractionofAltocumulusand Estimation 88 LowerCloudLayers 127 Contents ix 5.4. CirriformClouds 127 7.2. ThePressurePerturbationField 5.4.1. Nomenclature 127 AssociatedwithBuoyancy 166 5.4.2. ClimatologyandOriginsof 7.3. EntrainmentandDetrainment 167 CirriformClouds 128 7.3.1. GeneralConsiderations 167 5.4.3. Microphysics,VerticalAirMotions, 7.3.2. EarlyViewsofMixingwith andRadiationCirriformClouds 130 theCloud’sEnvironment 168 5.4.4. SmallCirriformConvective 7.3.3. MoreRealisticViewsof Elements—“GeneratingCells” 132 EntrainmentandDetrainment 175 5.4.5. BuoyantAnvilDynamics 133 7.3.4. EffectofEntrainmentonBuoyancy 5.4.6. RadiativeDestabilizationand andDownwardMotionNear ShearEffectsonaLayerof CloudEdge 176 CirriformCloud 137 7.3.5. LateralVersusCloud-Top 5.4.7. MesoscaleCirculationInducedBy Entrainment 176 RadiativeHeatingofaLayer 7.3.6. ConvectiveCloudinaFixed ofCirriformCloud 138 Column 177 7.3.7. RepresentationofMixingin 6. Nimbostratus and the Separation MultidimensionalModelsof of Convective and Stratiform ConvectiveClouds 180 Precipitation 141 7.3.8. RepresentationofConvective CloudsinLargeScaleModels 6.1. DefinitionofStratiformPrecipitation oftheAtmosphere 182 andHowItDiffersfromConvective 7.4. VorticityandDynamicPressure Precipitation 142 PerturbationForces 182 6.2. TheContrastingRadar-EchoStructures 7.4.1. TheVorticityApproachto ofStratiformandConvective UnderstandingRotationand Precipitation 144 DynamicPressureinConvective 6.3. MicrophysicalObservationsin Clouds 182 NimbostratusandImpliedVertical 7.4.2. HorizontalVorticity 182 AirMotions 146 7.4.3. VerticalVorticityIntroducedby 6.4. RoleofConvectioninRegions TiltingofEnvironmentalHorizontal ofStratiformPrecipitation 147 Vorticity 183 6.5. StratiformPrecipitationwithShallow 7.4.4. EffectsofVorticesonEntrainment OverturningConvectiveCellsAloft 147 andPressurePerturbation 183 6.6. StratiformPrecipitationProduced byDeepConvection 152 8. Cumulonimbus and Severe Storms 6.6.1. ParticleFountainsandthe 187 EvolutionofDeepConvective 8.1. TheBasicCumulonimbusCloud 187 CellsintoNimbostratus 152 8.2. MulticellStorms 190 6.6.2. StratiformPrecipitationProduced 8.3. SupercellStorms 194 byDiscreteRedevelopment 8.4. EnvironmentalConditionsFavoring ofDeepConvection 154 DifferentTypesofDeepConvective 6.6.3. StratiformPrecipitationProduced Storms 198 byConvectiveRedevelopment 8.5. SupercellDynamics 203 inaVariousWindShear 8.5.1. StormSplittingandPropagation 203 Environments 156 8.5.2. DirectionalShearinthe 6.6.4. MicrophysicsoftheStratiform Environmentofthe PrecipitationAssociatedwith CumulonimbusCloud 204 DeepConvectiveClouds 157 8.5.3. UpdraftRotation 205 6.7. RadiativeEffectsonNimbostratus 161 8.5.4. HelicityandtheStrengthof 6.8. SeparationofConvectiveandStratiform SupercellUpdraftRotation 207 Precipitation 162 8.5.5. BaroclinicityAssociatedwith 7. Basic Cumulus Dynamics Downdrafts 207 165 8.5.6. TheThreeSourcesofRotation 7.1. Buoyancy 165 inaSupercell 207

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