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Subject Item
dbpedia:Climate_of_Asia
rdfs:comment
The Climate of Asia is wet across southeast sections, and dry across much of the interior. Some of the largest daily temperature ranges on Earth occur in western sections of Asia. The monsoon circulation dominates across southern and eastern sections, due to the presence of the Himalayas forcing the formation of a thermal low which draws in moisture during the summer. Southwestern sections of the continent are hot.
rdfs:seeAlso
dbpedia:Tropical_cyclone
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