Question

WHAT KIND OF QUESTIONS CAN BE EXPECTED FROM THIS PASSAGE ?

The monsoons are experienced in the
tropical area roughly between 20° N and 20°
S. To understand the mechanism of the
monsoons, the following facts are important.
(a) The differential heating and cooling of
land and water creates low pressure on the
landmass of India while the seas around
experience comparatively high pressure.
(b) The shift of the position of Inter Tropical
Convergence Zone (ITCZ) in summer, Over
the Ganga plain (this is the equatorial trough
normally positioned about 5°N of the
equator. It is also known as the monsoon-
Arough during the monsoon season).
(c) The presence of the high-pressure area,
east of Madagascar, approximately at
20°S over the Indian Ocean. The intensity
and position of this high-pressure area
affects the Indian Monsoon.
(d) The Tibetan plateau gets intensely
heated during summer, which results in
strong vertical air currents and the
formation of low pressure over the plateau
at about 9 km above sea level.
(e) The movement of the westerly jet stream
to the north of the Himalayas and the
presence of the tropical easterly jet
stream over the Indian peninsula during
Summer




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Answer 1

the _ pleateau gets intensely heated during summer

Answer 2

Answer:

The monsoons are experienced in the

tropical area roughly between 20° N and 20°

S. To understand the mechanism of the

monsoons, the following facts are important.

(a) The differential heating and cooling of

land and water creates low pressure on the

landmass of India while the seas around

experience comparatively high pressure.

(b) The shift of the position of Inter Tropical

Convergence Zone (ITCZ) in summer, Over

the Ganga plain (this is the equatorial trough

normally positioned about 5°N of the

equator. It is also known as the monsoon-

Arough during the monsoon season).

(c) The presence of the high-pressure area,

east of Madagascar, approximately at

20°S over the Indian Ocean. The intensity

and position of this high-pressure area

affects the Indian Monsoon.

(d) The Tibetan plateau gets intensely

heated during summer, which results in

strong vertical air currents and the

formation of low pressure over the plateau

at about 9 km above sea level.

(e) The movement of the westerly jet stream

to the north of the Himalayas and the

presence of the tropical easterly jet

stream over the Indian peninsula during

Summer