University Clearing through UCAS. You can apply for other courses through Clearing if you donât get a place on your chosen university course. You may still get a place on one of your chosen courses if you miss your grades by a narrow margin. Who can use Clearing.
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 Water Circulation. Deep waters are formed where the air temperatures are cold and where the salinity of the surface waters are relatively high. The combinations of salinity and cold temperatures make the water denser and cause it to sink to the bottom.The Gulf Stream carries salt into the high latitude North Atlantic where the water cools. The cooling and the added salt cause the waters to sink in the Norwegian Sea.This is the formation of Atlantic Deep Water. Places where the water is cold enough and salty enough to form bottom water.Links. Links. 1. Deep Water. 2.he combinations of salinity and cold temperatures make the water denser and cause it to sink to the bottom. The Gulf Stream carries salt into the high latitude North Atlantic where the water cools. The cooling and the added salt cause the waters to sink in the Norwegian Sea.