Warm water can carry more salt than cold water can.
Probable because the solubilty of salt is higher.
Deep ocean currents and surface currents do meet, but mixing is limited. The waters stratify based on temperatures and salinity. The higher the salinity, the heavier the water.
What causes low salinity in the oceans at high latitudes?In subtropical latitudes, high surface evaporation creates high salinity near the sea surface. In subpolar latitudes, high precipitation creates low salinity near the sea surface. As these waters flow into the ocean interior, they create layers of high and low salinity.
The salinity of ocean water depends on its location, rate of evaporation, amount of precipitation and amount of freshwater added to the ocean.
This source is ocean waters.
Surface water slainity is higher in tropical regions.
Deep ocean currents and surface currents do meet, but mixing is limited. The waters stratify based on temperatures and salinity. The higher the salinity, the heavier the water.
What causes low salinity in the oceans at high latitudes?In subtropical latitudes, high surface evaporation creates high salinity near the sea surface. In subpolar latitudes, high precipitation creates low salinity near the sea surface. As these waters flow into the ocean interior, they create layers of high and low salinity.
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Surface water salinity ranges from 32 to 37 parts per 1000
The Antarctic Intermediate Water (AAIW) are the low salinity waters found in the Southern Ocean.
Surface water salinity ranges from 32 to 37 parts per 1000
The salinity of ocean water depends on its location, rate of evaporation, amount of precipitation and amount of freshwater added to the ocean.
Surface waters make up about 10% of all the water in the ocean.
This source is ocean waters.
Salinity is the saltiness or dissolved salt content of a body of water. The average ocean salinity is 35 ppt. This number varies between about 32 and 37 ppt. Rainfall, evaporation, river runoff, and ice formation cause the variations. For example, the Black Sea is so diluted by river runoff, its average salinity is only 16 ppt. Freshwater salinity is usually less than 0.5 ppt. Water between 0.5 ppt and 17 ppt is called brackish. Estuaries, where fresh river water meets salty ocean water, are examples of brackish waters. Saline waters from inland seas can have a composition that differs from that of the ocean.
Ocean water off the Antarctic coast is between 32F degrees and about 27F degrees, based on the salinity of the water. It's always warmer in the ocean water than it is above the surface of the water.
Surface water slainity is higher in tropical regions.