Water both heats up and cools down at a slower rate than land.
Atlantic ocean has a lower average temperature
The difference in temperature between the ocean and the sand is primarily due to the difference in their heat absorption capacities. Water has a higher specific heat capacity compared to sand, so it heats up and cools down more slowly. As a result, the ocean retains heat for longer periods of time compared to sand, leading to differences in temperature between the two.
Ocean currents are dure to a cobination of wind, the Corilis effect, and temperature differences.
Breezes are created when there are specific heat differences between land and ocean.
There are many different forces that create ocean currents. Among them are: the earth's rotation, salinity differences, wind, density differences, and buoyant forces. Temperature differences can create some of these differences, but we would have ocean currents even if the oceans were a uniform temperature.
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The Southern Ocean is the ocean surrounding Antarctica. The Pacific Ocean is the ocean between Asia/Oceania and the Americas.
Temperature differences between the equator and the poles drive atmospheric circulation and ocean currents, leading to the creation of weather patterns and climate zones. These differences play a key role in shaping global climate and help redistribute heat around the Earth.
Differences in temperature and in density of seawater drive deep ocean currents.
Deep ocean currents are caused by differences in saltiness or water temperature.
mechanical
Breezes are created when there are specific heat differences between land and ocean.