Physical Processes
Monsoon Circulation
Also Known As Monsoon
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A monsoon is a seasonal reversal of wind and rainfall driven by the unequal way land and ocean heat and cool through the year and by the annual swing of the Intertropical Convergence Zone that follows. Heated land draws in moist ocean air that rises and falls as rain; the pattern reverses with the seasons. The South Asian, East Asian, West African and Australian monsoons are the world's principal systems, and in India alone the summer monsoon supplies close to eighty percent of annual rainfall for an agricultural sector employing most of the population.
Facts
Process TypeAtmospheric Circulation 1 TimescaleAn annual cycle, reversing between wet and dry seasons roughly twice a year. 1 First Proposed Year Cross-Tradition Connections
Demonstrated By
The South Asian summer monsoon supplies close to eighty percent of India's annual rainfall.
Sources
1. Monsoon (Wikipedia)
Wikimedia FoundationDefinition sectionQuote, Definition section
A monsoon is a seasonal reversing wind accompanied by corresponding changes in precipitation.
View the Source 2. Edmond Halley (Wikipedia)
Wikimedia FoundationScientific work sectionQuote, Scientific work section
In this article he identified solar heating as the cause of atmospheric motions.
View the Source East Asian Monsoon (Wikipedia)
Wikimedia FoundationDemonstrated By: East Asia, Lead sectionQuote, Demonstrated By: East Asia, Lead section
The East Asian monsoon is a monsoonal flow that carries moist air from the Indian Ocean and Pacific Ocean to East Asia.
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