Definitions
from The American Heritage® Dictionary of the English Language, 5th Edition.
- noun An intermediate layer of oceanic water in which salinity increases more rapidly with depth than in the layers above and below it.
from Wiktionary, Creative Commons Attribution/Share-Alike License.
- noun a strong, vertical salinity gradient; the (sometimes indistinct) border between layers of water that contain different amounts of
salt
Etymologies
from Wiktionary, Creative Commons Attribution/Share-Alike License
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Examples
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They're filled with fresh water (though there are areas where the salt water comes in and creates a salt / fresh water interface called the halocline, which looks wicked cool.
doggdot.us 2008
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Freshwater is stored in the surface and halocline layers of the marine Arctic.
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Regionally, the effects of upwelling of halocline waters onto the shelf must also be considered.
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Modification of halocline source waters during freezing on the Beaufort Sea shelf: evidence from oxygen isotopes and dissolved nutrients.
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Brine release during sea-ice formation increases the density of surface waters which then sink and are advected from the shelf to basin interiors, transporting CO2 into the halocline and deeper waters.
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Furthermore, the role that lateral advection plays in establishing the underlying halocline structure of the Arctic Ocean must also be considered.
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Waters below the halocline are modified Atlantic waters that flowed into the Arctic through Fram Strait and the Barents Sea.
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Low salinity waters are added to the surface and halocline layers via precipitation and runoff, Pacific inflow via the Bering Strait, and the sea-ice distillation process.
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The layer containing the greatest change in salinity is called the halocline.
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In the Arctic Ocean, freshwater is stored within the various layers above and within the halocline, the latter serving as an extremely complex and poorly understood reservoir.
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