Explain why Delhi receives very light rainfall in Fig.
4. [4]
-
Delhi receives
light rainfall due to northeast monsoon (October – February)
-
an area of high
pressure forms overs Indian sub-continent and Central Asia while an area of low
pressure forms over Australia
-
due to differences
in pressure between the northern and southern hemispheres, air moves from
Central Asia down towards Indian sub-continent
-
resulting in drier
and colder winds that bring with it light rainfall as they blow across cold
land to Delhi
With reference to Fig.
6, explain how Mangalore, India is affected by Southwest monsoon.
[4]
·
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.
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Sunday, January 31, 2016
Answers to Monsoon wind P62
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