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Confidence votes 77.6K. The basic differences are that the deep water wave spreads out and moves very quickly across open water. Wave height is not significant in these waves. When the wave reaches shallow water, however, it slows down at the leading edge.This causes the wave to bunch up and increase in height, even to dangerous proportions.he basic differences are that the deep water wave spreads out and moves very quickly across open water.
Deep-ocean flow (and, to a lesser extent, surface flow) is driven by density differences produced by heating and cooling and by precipitation and evaporation (cool saline water is denser than warm fresh-water). The behaviour of the atmosphere strongly affects these density differences.