Horizontal motion of atmosphere does not include
1.Planetary circulations
2. Synoptic.circulations
3.Meso scale motions
4.Trade winds
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Pacific North America (PNA)
Atmospheric circulation variability over the extratropical Pacific is partially dominated by Rossby wave patterns originated in the subtropical western Pacific, associated with anomalous tropical heating [26]. The wave-like pattern that propagates towards the North American Continent is known as PNA pattern, similarly its southern hemisphere counterpart become known as the Pacific-South American
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