The air circulation over the oceans in the middle latitudes is mainly anticyclonic [Sub-tropical High Pressure Belt] (more pronounced in the southern hemisphere than in the northern hemisphere due to differences in the extent of landmass). The oceanic circulation pattern also corresponds with the same.
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Ocean currents: Forces Responsible For Ocean Currents | Desert Formation and Ocean Currents | PMF IASonsoon winds are responsible for the seasonal reversal of ocean currents in the Indian ocean. The oceanic circulation pattern roughly corresponds to the earth’s atmospheric circulation pattern. <span>The air circulation over the oceans in the middle latitudes is mainly anticyclonic [Sub-tropical High Pressure Belt] (more pronounced in the southern hemisphere than in the northern hemisphere due to differences in the extent of landmass). The oceanic circulation pattern also corresponds with the same. At higher latitudes, where the wind flow is mostly cyclonic [Sub-polar Low Pressure Belt], the oceanic circulation follows this pattern. In regions of pronounced monsoonal flow [Norther Summary
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