NettetLife that has adapted to these extreme regions – including sea ice-dependent species from tiny algae to huge polar bears – is being impacted. Salinity is a "key ingredient" for high-latitude ocean ecological communities. Why? It affects seawater density which, in turn, influences the movement of water, heat, and carbon. NettetWhere does ocean water go? All this heating and cooling and melting and thawing creates a layered ocean: warmer fresher water on top, cold salty water at the bottom. Organisms move from one layer to another, and plant and animal remains containing nutrients "rain" down, but the layers stay fairly separate in all but a few places.

"Ocean currents result from two processes: the wind on the

Nettet1. sep. 2011 · Description. The ocean is not a still body of water. There is constant motion in the ocean in the form of a global ocean conveyor belt due to thermohaline currents. These currents are density driven, which are affected by both temperature and salinity. Cold, salty water is dense and sinks to the bottom of the ocean while warm water is … Netteta body of water within an ocean or lake with similar salinity, temperature, and density. salinity. the degree of saltiness of a salt solution, especially applied to ocean water. … download fnaf special delivery

Oceans and Seas and the Water Cycle U.S. Geological Survey

Nettet6. Cold, salty water is more dense. Cold water is more dense than warm water. Salty water is more dense than less salty water. 7. Answers may vary but should show that students understand that winds and the Coriolis effect also influence surface current patterns. Possible answer: Surface currents would flow along curved paths because the NettetFormation and circulation. Antarctic bottom water is created in part due to the major overturning of ocean water. Antarctic bottom water is formed in the Weddell and Ross Seas, off the Adélie Coast and by Cape Darnley … Nettet5. apr. 2024 · It occurs through a process known as thermohaline circulation, which involves the movement of cold, dense water to the ocean depths due to differences in temperature and salinity. Deep water formation typically occurs in regions of upwelling, downwelling, or cyclonic flow in the ocean, such as near the poles, along the oceanic … clarkys bacon snack