bottom water वाक्य
उदाहरण वाक्य
मोबाइल
- In the deepest parts of the sea, the bottom waters were saltier than the top, and not mixing.
- Gas saturates the bottom water and stays trapped there, like the carbon dioxide in a sealed bottle of seltzer.
- The algae settles in the bottom waters and decays, consuming oxygen faster than it can be replenished from the surface.
- Antarctic bottom water is formed in the Cape Darnley from surface water cooling in polynyas and below the ice shelf.
- Oxygen depletion in bottom waters then favours the enhanced preservation of the sinking organic matter during burial in the sediments.
- This colder bottom water hits a warmer surface layer that is eutrophied, awash in algae due to the nitrogen-rich runoff.
- One of these is the Antarctic Bottom Water, a very cold, highly saline, dense water that forms under sea ice.
- Atlantic Water has the same salinity as Arctic Bottom Water but is much warmer ( up to 3 �C ).
- Just as river valleys direct streams and rivers on the continents, the bottom topography steers the deep and bottom water masses.
- There were sea-going generator designs based on thermodynamics, which exploited the temperature difference between warm surface water and cold bottom water.
- Lake Erie is the shallowest of the Great Lakes and seldom overturns enough to bring the cold bottom water to the surface.
- Underlying these oxygenated waters and separated by a pycnocline, were anoxic and hypersaline bottom waters, which preserved organic matter as it accumulated.
- Authorities now hope fall storms, that would re-oxygenate the bottom water through mixing with oxygen-rich surface water, will sweep across the region.
- Bottom waters flow very slowly, driven mainly by slope topography and differences in temperature and salinity, especially compared to wind-driven surface ocean currents.
- In 2014 two degassing pipes, similar to those operating in lake Nyos, were installed to decrease the gas pressure at the bottom waters.
- On the shelf, bottom waters exhibit characteristics of the central Indian Ocean in the east and central Atlantic Ocean waters in the west.
- Naturally there is also a bottom water stratification between semi-ventilated deep water ( uninhabitable but not rotten ) and totally isolated poisonous bottom water.
- This Antarctic wind is stronger during the winter months and thus the Antarctic bottom water formation is more pronounced during the Antarctic winter season.
- Subsurface productivity is limited by nutrient availability, as the anoxic bottom waters act as a sink for reduced nitrate, in the form of ammonia.
- Spawning occurs from July until September at a bottom water temperature of 22 26 �C . Spawning is related to water temperature and salinity.
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