Climateisthelong-termaverageofweather,
typicallyaveragedoveraperiodof30years.Someofthe
meteorologicalvariablesthatarecommonlymeasured
aretemperature,humidity,atmosphericpressure,wind,
andprecipitation.Inabroadersense,climateisthestate
ofthecomponentsoftheclimatesystem,whichincludes
theoceanandiceonEarth.Theclimateofalocationis
affectedbyitslatitude,terrain,andaltitude,aswellas
rents.
Weatheristhestateoftheatmosphere,
describingforexamplethedegreetowhichitishotor
cold,wetordry,calmorstormy,clearorcloudy.Most
weatherphenomenaoccurinthelowestlevelofthe
atmosphere,thetroposphere,justbelowthe
stratosphere.Weatherreferstoday-to-day
temperatureandprecipitationactivity,whereas
climateisthetermfortheaveragingofatmosphericconditionsoverlongerperiodsoftime.
Whenusedwithoutqualification,"weather"isgenerallyunderstoodtomeantheweatherof
Earth.Weatherisdrivenbyairpressure,temperatureandmoisturedifferencesbetween
oneplaceandanother.OnEarth,thecommonweatherphenomenaincludewind,cloud,
rain,snow,fogandduststorms.Lesscommoneventsincludenaturaldisasterssuchas
tornadoes,hurricanes,typhoonsandicestorms.Almostallfamiliarweatherphenomena
occurinthetroposphere(thelowerpartoftheatmosphere).
Climate and Weather
Weatherreferstoshort-termchangesintheatmosphere,climatedescribeswhattheweatherislikeovera
longperiodoftimeinaspecificarea.Differentregionscanhavedifferentclimates.Example,weathertells
youwhattoweareachday.Climatetellsyouwhattypesofclothestohaveinyourcloset.
nearbywaterbodiesandtheircur
Thestandardaveragingperiodis30years,butotherperiodsmaybeuseddependingon
thepurpose.Climatealsoincludesstatisticsotherthantheaverage,suchasthe
magnitudesofday-to-dayoryear-to-yearvariations.Thereareseveralwaystoclassify
climatesintosimilarregimes.Originally,climesweredefinedinAncientGreecetodescribe
theweatherdependinguponalocation'slatitude.Modernclimateclassificationmethods
canbebroadlydividedintogeneticmethods,whichfocusonthecausesofclimate,and
empiricmethods,whichfocusontheeffectsofclimate.
TheKöppenclassificationdependsonaveragemonthlyvaluesoftemperatureand
precipitation.ThemostcommonlyusedformoftheKöppenclassificationhasfiveprimary
typeslabeledAthroughE.TheseprimarytypesareA)tropical,B)dry,C)mildmid-latitude,
D)coldmid-latitude,andE)polar.Thefiveprimaryclassificationscanbefurtherdivided
intosecondaryclassificationssuchasrainforest,monsoon,tropicalsavanna,humid
subtropical,humidcontinental,oceanicclimate,Mediterraneanclimate,desert,steppe,
subarcticclimate,tundra,andpolaricecap.
Y d Confusion The Book of Knowledge 152
YtheCONFUSION