Definitions
from The American Heritage® Dictionary of the English Language, 5th Edition.
- noun An intermediate layer of oceanic water in which density increases more rapidly with depth than in the layers above and below it.
from Wiktionary, Creative Commons Attribution/Share-Alike License.
- noun A
boundary layer in a body ofwater between areas of differenttemperature orsalinity . - noun A layer of water where the
density changes rapidly withdepth
Etymologies
from The American Heritage® Dictionary of the English Language, 4th Edition
from Wiktionary, Creative Commons Attribution/Share-Alike License
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Examples
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Near the pycnocline (i.e., the region of strongest vertical density gradient) in arctic waters, a restricted vertical supply of nutrients enables the development of a 3 to 10 m thick chlorophyll maximum layer that is strongly light-limited [21].
Physical factors mediating ecological change in the Artic 2009
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Pulsed (wind-driven) nutrient supplies associated with passing atmospheric low pressure systems often result in small blooms, however, in arctic waters, the pycnocline is usually too strong to allow a temporary deepening of the surface mixed layer and so bring in nutrients from sub-pycnocline waters [24].
Physical factors mediating ecological change in the Artic 2009
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Heat flows downward across the pycnocline causing formation of frazil ice in the lower part of the fresh layer.
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Fresh water enters the fiord in the form of melt streams which flow down to the pycnocline.
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Hypoxia occurs below the freshwater driven pycnocline from late February through early October, but it is most widespread, continuous, and severe in June, July, and August.
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Iron particles and soluble iron had been carried there along a layer of denser water roughly 100 to 150 meters deep (the pycnocline), and the iron had been stirred up by storms that made it available to near-surface plankton in the dead of winter. "
RealClimate 2009
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