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What is rain?
Rainis liquidwaterinthe formof dropletsthathave condensedfromatmosphericwatervaporand
thenprecipitated—thatis,becomeheavyenoughtofall undergravity.Rainisamajor componentof
the watercycle and is responsible fordepositingmostof the freshwateronthe Earth. It provides
suitable conditionsformanytypesof ecosystems,aswell aswaterforhydroelectricpowerplantsand
crop irrigation.
The major cause of rainproductionismoisture movingalongthree-dimensionalzonesof
temperature andmoisture contrastsknownasweatherfronts.If enoughmoisture andupward
motionispresent,precipitationfallsfromconvectiveclouds(thosewithstrongupwardvertical
motion) suchas cumulonimbus(thunderclouds) whichcanorganize intonarrow rainbands.In
mountainousareas,heavyprecipitationispossiblewhere upslopeflow ismaximizedwithin
windwardsidesof the terrainatelevationwhich forcesmoistairtocondense andfall outas rainfall
alongthe sidesof mountains.Onthe leewardside of mountains,desertclimatescanexistdue tothe
dry air causedbydownslope flow whichcausesheatinganddryingof the air mass.The movementof
the monsoontrough,or intertropical convergence zone,bringsrainyseasonstosavannahclimes.

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What is rain

  • 1. What is rain? Rainis liquidwaterinthe formof dropletsthathave condensedfromatmosphericwatervaporand thenprecipitated—thatis,becomeheavyenoughtofall undergravity.Rainisamajor componentof the watercycle and is responsible fordepositingmostof the freshwateronthe Earth. It provides suitable conditionsformanytypesof ecosystems,aswell aswaterforhydroelectricpowerplantsand crop irrigation. The major cause of rainproductionismoisture movingalongthree-dimensionalzonesof temperature andmoisture contrastsknownasweatherfronts.If enoughmoisture andupward motionispresent,precipitationfallsfromconvectiveclouds(thosewithstrongupwardvertical motion) suchas cumulonimbus(thunderclouds) whichcanorganize intonarrow rainbands.In mountainousareas,heavyprecipitationispossiblewhere upslopeflow ismaximizedwithin
  • 2. windwardsidesof the terrainatelevationwhich forcesmoistairtocondense andfall outas rainfall alongthe sidesof mountains.Onthe leewardside of mountains,desertclimatescanexistdue tothe dry air causedbydownslope flow whichcausesheatinganddryingof the air mass.The movementof the monsoontrough,or intertropical convergence zone,bringsrainyseasonstosavannahclimes.