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The Indian Monsoon

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The Indian Monsoon ATS 553 Geography Lesson Reversal of the Winds Most dramatic seasonal reversal of the winds in the world. Northern Summer Flow _at_ SFC Northern ... – PowerPoint PPT presentation

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Title: The Indian Monsoon


1
The Indian Monsoon
  • ATS 553

2
Geography Lesson
Himalayas/Tibetan Plateau
Afghanistan
Pakistan
Indian Subcontinent
Arabian Sea
Bay of Bengal
3
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4
Reversal of the Winds
  • Most dramatic seasonal reversal of the winds in
    the world.

5
Northern Summer Flow _at_ SFC
"Southwest Monsoon"
6
Northern Winter Flow _at_ SFC
"Northeast Monsoon"
7
SST in the Arabian Sea
8
SST in the Arabian Sea
0 90 180 270 0
Wind Direction Notice the shift in direction
with the onset of the southwest monsoon.
9
SST in the Arabian Sea
0 90 180 270 0
Wind Speed Notice that the southwest Monsoon
(summer) is much stronger than the northeast
monsoon.
10
SST in the Arabian Sea
0 90 180 270 0
Temperature Once the southwest monsoon begins,
SST begins to fall, despite the fact that it is
June!
11
SST in the Arabian Sea
0 90 180 270 0
Heat Flux During the southwest monsoon, heat
flux is often negative due to huge amounts of
evaporation!
12
Positive Feedback in the Winds
  • In the Summer
  • Continent heats up more than the oceans do.
  • Strong flow from the ocean towards the land.
  • Very strong flow results in greater mixing in the
    Arabian Sea.
  • Therefore, SSTs fallArabian Sea is actually
    COLDER in the summer than it is in the winter!
  • Results in even stronger monsoon flow!

13
Onset/Withdrawal Dates
14
Monsoon Trough Location
15
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16
Extremely high temperatures in northern India and
Southern Pakistan.
17
A strong heat low!
18
Extremely high dewpoints in northern India and
Southern Pakistan. Notice Myanmar!
19
Why is the Southwest Monsoon so much stronger
than the Northeast Monsoon?
20
To have a strong winter monsoon
  • you need the continent to cool down in the
    winter.
  • Best accomplished by cold air outbreaks from the
    north.

21
The Himalayas are in the way!
22
Seasonality
  • In Summer
  • The continent heats up a lot.
  • Feedbacks keep SSTs low.
  • Southwest monsoon is strong.
  • In Winter
  • The continent doesnt cool down all that much.
  • SSTs arent particularly warm.
  • Northeast monsoon is weak.

23
Southeast Asian Monsoon
  • Which is why the winter monsoon is so strong in
    southeast asia!

24
(No Transcript)
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