Sea Floor Temperature North Sea

Besides water temperature you can also get information about the weather for today tomorrow and the upcoming days surf forecast as well as the data on sunrise sunset and moonrise moonset at a given point on any given day.

Sea floor temperature north sea.

Interaction with the wind keeps this layer mixed and thus allows the heating from the sun to be distributed vertically. Weddell sea bottom water wsbw is a subset of antarctic bottom water aabw that is at a temperature of 0 7 c or colder. Current north sea water temperature map. This process is known as thermohaline circulation.

Select it from the side menu at left or select it from a google map based web page or. The sea floor then drops off steeply along the continental slope the true edge of the continent. The average temperature of the ocean surface water is about 17 c 62 6 f 17 c. The sea surface temperatures range from as high as 97 f 36 c in the persian gulf to 28 f 2 c near the north pole.

It originates in the weddell sea and closely follows the sea floor as it flows out into the rest of the world s oceans. It is created mainly due to the high surface winds blowing off the antarctic. To see the details select the country and then the city of your interest. The following features are shown at example depths to scale though each feature has a considerable range at which it may occur.

This data the surface water temperature on the north sea coast. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. Coastal water temperature guide cwtg to display water temperatures in a region of your interest. Temperature of ocean water university of michigan.

World water temperature from global sea temperatures. Look at figure 14 23. It consists of a higher salinity branch and a lower salinity branch. It is estimated that 92 per cent of the entire sea floor has a temperature lower than 40 degrees fahr 4 5 c.

The smooth flat regions that make up 40 of the ocean floor are the abyssal plain. If you follow the ocean floor out from the beach at the top left the seafloor gently slopes along the continental shelf. Continental shelf 300 feet continental slope 300 10 000 feet abyssal plain 10 000 feet abyssal hill 3 000 feet up from the abyssal plain seamount 6 000 feet. Differences in water density resulting from the variability of water temperature thermo and salinity haline also cause ocean currents.