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The most possible explanation for the location of the Thar Desert in western India is
The Thar Desert lies in the leeward side of the Aravalis and hence no rain bearing winds are able to reach Thar.
The absence of Mountains to the North or West of Thar to cause orographic rains.
The moisture carried by the southwest monsoon is driven away by dry convectional currents.
None of the above
2nd option is correct. The most possible explanation for the location of the Thar Desert in western India is the absence of Mountains to the North or West of Thar to cause orographic rains.
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