Page 130 - SST Class 06
P. 130

WHAT CAUSES THE SEASONS?                         extratropical  (non-tropical)  cyclone  formation

             The seasons are caused by the tilt of the earth’s      (low pressure). These storms are thus much more
             rotational  axis  away  or  toward  the  sun  as  it   frequent  and  intense  in  the  winter  than  in  the
             travels through its year-long path around the sun.     summer.
             The earth has a tilt of 23.5 degrees relative to the
             “ecliptic plane” (the imaginary surface formed by
             its almost-circular path around the sun). The tilt
             toward  the  sun  is  maximized  during  Northern
             Hemisphere  summer  in  late  June  (the  "summer
             solstice").  At  this  time,  the  amount  of  sunlight
             reaching the Northern Hemisphere is at a maxi-
             mum.
             In  late  December,  on  the  date  of  the  “winter
             solstice”,  the  earth’s  tilt  away  from  the  sun  is
             maximized,  leading  to  a  minimum  of  sunlight                        Winter Solstice
             reaching the Northern Hemisphere. The seasons,
             of  course,  are  reversed  in  the  Southern
             Hemisphere.
             During the winter, cold air masses  build up over
             North America, Europe and Asia, due to the low
             intensity of sun light. The oceanic air masses are
             much  less  affected  by  the  seasons  because
             circulations  in  the  upper  ocean  replenish  warm
             surface water if it has been cooled.
             The  strong  temperature  contrast  between  the
             cold  air  masses  over  land  and  the  relatively
                                                                                     Summer Solstice
             warmer  air  masses  over  the  ocean  lead  to

              Terminology

              Inclination     :  degree of sloping
              Equinoxes       :  one of the two days in the year when day and night are of equal length
              Replenish       :  fill up again


             Inside Story
             Inside Story
              g  The earth rotates on its axis everyday and orbits the sun every year.
              g  The tilting of the earth on its axis is known as the inclination of the earth’s axis.
              g  It takes the earth just under 24 hours to make one complete rotation.

              g  Being  spherical  in  shape,  the  earth  completes  one  motion  in  24  hours  and  moves  from
                  west to east.
              g  The circle which divides the earth into lit-half is known as circle of illumination.


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