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Biology, 12.12.2020 17:00 emilyborland50

Latitudinal differences in surface warming give rise to global patterns of air circulation and rainfall. At the equator and the latitudes of 60 degrees . At the poles and the latitudes of 30 degrees . A. cold, dry air sinks; warm, moist air rises and loses moisture as rain
B. warm, moist air rises and loses moisture as rain; cold, dry air sinks

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