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water.  Droplets  joining  together  form  bigger           when warm air meets cold air. Stratiform
             drops. Huge masses of water droplets are called             rainfall usually occurs from nimbostratus
             ‘clouds’.                                                   cloud.

             When these droplets become too heavy to float          3.  Relief or Orographic Rainfall
             in  the  air,  they  come  down  as  ‘precipitation’,       Orographic
             Precipitation  is  of  different  types.  That,  which      rainfall occurs
             comes down to the earth in liquid form is called            when a mass of
             rain.  The  other  forms  are  snow,  sleet  and  hail.     air is pushed up
             Rainfall is the main source of groundwater which            because of a
             is very important for the vegetation-cover on the           structure with
             earth  surface.  It  is  also  an  important  source  of    very high eleva-
             fresh  water.  Very  tiny  drops  of  rain  water  are      tion such as a
             called  drizzle.  The  instrument  used  to  measure        mountain. The
             rainfall is called the rain gauge.                          lifted air cools down and precipitation
             Rainfall itself is of three types :                         occurs. Rain shadow area is formed on the
             Convectional, Cyclonic or Stratiform and Relief             other side of the elevation.
             or Orographic rainfall.                                Rainfall  is  extremely  important  for  existence  of
             1.  Convectional Rainfall                              life on the earth. It is not only a source of fresh
                  When  a  portion  of                              water, it also effects the vegetation of any area.
                  the  earth  becomes                                              AIR POLLUTION
                  heated  more  than                                Any change in the composition of air is termed
                  its  surrounding,  it                             as air pollution. It results from release of certain
                  creates  significant                              gaseous, solid or liquid agents in the atmosphere.
                  amount of evapora-                                The obvious causes of air pollution are—growing
                  tion.  Convection                                 industrial  activity,  excessive  burning  of  fossil
                  currents  then  push                              fuels,  rising  numbers  of  automobiles,  fires  and
                  up the moist air and                              burning of solid wastes. The chief air pollutants
                  cumulonimbus  clouds  are  formed.  These         are – carbon dioxide, carbon monoxide, chloro-
                  clouds  result  in  convectional  rainfall.       fluorocarbons,  suspended  particulate  matter,
                  Convectional  rainfall  is  in  the  form  of     sulphur dioxide, nitrogen oxide and lead.
                  showers with rapidly changing intensity. This     Air  pollution  leads  to  serious  health  problems
                  type of rainfall happens for a short duration     such  as  loss  of  biodiversity  and  damage  to
                  because  horizontal  expanse  of  a  cumulo-      historical monuments. It is a serious environmen-
                  nimbus cloud is small.                            tal problem and must be tackled urgently.
             2.  Cyclonic or                                        Greenhouse Gases and Ozone
                  Stratiform Rainfall
                                                                    Gases  like  water  vapor,  carbon  dioxide  and
                  This type of rainfall is
                                                        Warm air    methane are greenhouse gases which are present
                  formed by frontal          Cold air               in  the  small  amounts.  Like  a  thick  blanket  that
                  system surrounding                                covers  the  earth,  they  are  especially  good  at
                  extratropical cyclones.                           trapping heat. And, because their concentrations
                  Cyclone is formed                                 are increasing due to human activity, more heat

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