Difference between southwest monsoon season and northeast monsoon season (5points each)?
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Q. Difference between southwest monsoon season and northeast monsoon season.
SOUTHWEST MONSOON
The southwestern summer time monsoons arise from july via september. Thethar desert and adjoining areas of the northern and relevant indian subcontinentheats up extensively for the duration of the new summers. This causes a low stress area over the northern and central indian subcontinent. To fill this void, the moisture-encumbered winds from the indian ocean rush in to the subcontinent. These winds, rich in moisture, are drawn towards the himalayas. The himalayas act like a excessive wall, blocking off the winds from passing into significant asia, and forcing them to upward thrust. As the clouds upward push their temperature drops and precipitation happens. Some regions of the subcontinent receive up to ten,000 mm (390 in) of rain yearly.
NORTHEAST MONSOON
Round september, with the sun rapid retreating south, the northern land mass of the indian subcontinent starts to cool off rapidly. With this air stress starts to construct over northern india, the indian ocean and its surrounding ecosystem nevertheless holds its warmth. This causes cold wind to comb down from the himalayas andindo-gangetic simple towards the sizable spans of the indian ocean south of thedeccan peninsula. This is referred to as the northeast monsoon or taking flight monsoon.
Even as journeying in the direction of the indian ocean, the dry bloodless wind picks up a few moisture from the bay of bengaland pours it over peninsular india and parts of sri lanka. Towns like chennai, which get much less rain from the southwest monsoon, receive rain from this monsoon. About 50% to 60% of the rain obtained with the aid of the kingdom oftamil nadu is from the northeast monsoon.
SOUTHWEST MONSOON
The southwestern summer time monsoons arise from july via september. Thethar desert and adjoining areas of the northern and relevant indian subcontinentheats up extensively for the duration of the new summers. This causes a low stress area over the northern and central indian subcontinent. To fill this void, the moisture-encumbered winds from the indian ocean rush in to the subcontinent. These winds, rich in moisture, are drawn towards the himalayas. The himalayas act like a excessive wall, blocking off the winds from passing into significant asia, and forcing them to upward thrust. As the clouds upward push their temperature drops and precipitation happens. Some regions of the subcontinent receive up to ten,000 mm (390 in) of rain yearly.
NORTHEAST MONSOON
Round september, with the sun rapid retreating south, the northern land mass of the indian subcontinent starts to cool off rapidly. With this air stress starts to construct over northern india, the indian ocean and its surrounding ecosystem nevertheless holds its warmth. This causes cold wind to comb down from the himalayas andindo-gangetic simple towards the sizable spans of the indian ocean south of thedeccan peninsula. This is referred to as the northeast monsoon or taking flight monsoon.
Even as journeying in the direction of the indian ocean, the dry bloodless wind picks up a few moisture from the bay of bengaland pours it over peninsular india and parts of sri lanka. Towns like chennai, which get much less rain from the southwest monsoon, receive rain from this monsoon. About 50% to 60% of the rain obtained with the aid of the kingdom oftamil nadu is from the northeast monsoon.
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