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The cold freshwater therefore floats on top and the halocline across which mixing tends to be weak [6] even under ice free conditions [7] and therefore protects the surface from the heat in the Atlantic water. [8] Under the Atlantic water layer is a deep layer of Arctic bottom water extending to the bottom of the ocean.
The final defined water mass in the Arctic Ocean is called Arctic Surface Water and is found in the depth range of 150–200 m (490–660 ft). The most important feature of this water mass is a section referred to as the sub-surface layer.
Upper AIW is defined to be a denser layer on top of the lower AIW, between surface cold water and the lower AIW, including water masses with temperature maximum to minimum. It is characterized by temperatures less than 2 °C in the salinity ranges from 34.7 to 34.9. [3] The upper AIW is usually found at 75~150m, overlain by Arctic Surface Water ...
Plot of temperature and salinity in the Arctic Ocean at 85,18 north and 117,28 east dated Jan. 1st 2010. [6] In the graphical representation, three layers can be discerned: About 50 m (160 ft) of low salinity water "swimming" on top of the ocean. The temperature is −1.8 °C (28.8 °F), which is very near to the freezing point. This layer ...
In the Arctic Ocean, warm and salty water from the Atlantic enters the Arctic basin and subducts beneath the colder and fresher waters of the upper Arctic. In some regions, also Pacific waters sit below the mixed layer and above the Atlantic layer. A thermocline is found at the top of the Atlantic Water layer. In that region, temperature and ...
The pycnocline is the transitory region between a surface layer of water (warmer and less dense) and deeper layer of water (colder and more dense). Mixing occurs across the pycnocline, driven primarily by waves and shear. A pycnocline is the cline or layer where the density gradient ( ∂ρ / ∂z ) is greatest within
The Arctic Ocean is surrounded by continents and has a few narrow, relatively shallow connections to the large ocean basins to the south. Large amounts of riverine fresh water as well as abundant nutrients (gelbstoff) flow into the Arctic basin from Siberian rivers. The widest continental shelf on the planet is found in the Arctic Ocean ...
A talik is a layer of year-round unfrozen ground that lies in permafrost areas. In regions of continuous permafrost, taliks often occur underneath shallow thermokarst lakes and rivers, where the deep water does not freeze in winter and thus the soil underneath does not freeze either. Sometimes closed, open, and through taliks are distinguished.