Two Indian stations at nearly the same latitude show very different rainfall totals; the strongest single control explaining this is
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Chapter 6: Climate of India – Concepts and Controls (Set-4)
If two stations have the same latitude but very different annual temperature range, the most likely reason is difference in
Continue readingChapter 6: Climate of India – Concepts and Controls (Set-3)
The monsoon is important for India mainly because it brings most of the country’s annual rainfall in a few months
Continue readingChapter 6: Climate of India – Concepts and Controls (Set-2)
A climate graph is mainly used to show the yearly pattern of temperature and rainfall for a place A Rock
Continue readingChapter 6: Climate of India – Concepts and Controls (Set-1)
Climate refers to the average pattern of weather conditions of a place over a long period A Hourly atmospheric change
Continue readingChapter 5: Peninsular River Basins (Set-5)
In downstream terms, the “left bank” of the Ganga means the bank on your left when you face A Downstream
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In the upper Himalayas, the Bhagirathi is treated as a main headstream because it rises from the A Gangotri glacier
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The commonly accepted source glacier for the Bhagirathi, an important headstream of the Ganga, is located at A Gangotri Glacier
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The Narmada flows between which two major ranges, giving the Narmada valley a clear physical identity A Aravalli and Shivalik
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In peninsular India, which river is a classic west-flowing rift valley river that drains into the Arabian Sea through an
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