With
reference to Fig. 6, explain how Mangalore, India is affected by Southwest
monsoon.
•Max
3 marks awarded only if student never make reference to Mangalore, India.
•Between
June and September, when it is summer in
the northern hemisphere. Air over Central Asia heats up, expands and rises,
forming a region of low
pressure
over the area.
•During
the same period, the southern
hemisphere
is experiencing winter.
The low temperature causes the air to be cold
and dense,
exerting a greater force on the earth’s surface. This results in an area of high pressure
over
Australia.
•Due
to the difference in pressure between Central Asia and Australia, air from
Australia moves to the Indian sub-continent and Central Asia as the southeast monsoon
winds. As the winds cross the Equator, the Coriolis effect
deflects the
winds to the right.
•These
winds become the southwest
monsoon
winds
and warm up as they head for Central Asia.
The warm air picks up moisture as
it travels over the Indian
Ocean and
brings heavy rain
to
the Mangalore, India.
No comments:
Post a Comment