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SlideshowReport

Sea and Land Breezes

Description
Mid latitudes
Air flow is interrupted by cyclones
Cells move west to east in the Northern Hemisphere
Create anticyclonic and cyclonic flow
Paths of the cyclones and anticyclones are associated with the upper-level airflow

Produced from temperature differences
Small scale winds
Types
Land and sea breezes
Mountain and valley breezes
Chinook and Santa Ana winds
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