- halocline, vertical zone in the oceanic water column in which salinity changes rapidly with depth, located below the well-mixed, uniformly saline surface water layer.www.britannica.com/science/halocline
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Halocline - Wikipedia
In oceanography, a halocline (from Greek hals, halos 'salt' and klinein 'to slope') is a cline, a subtype of chemocline caused by a strong, vertical salinity gradient within a body of water. Because salinity (in concert with temperature) affects the density of seawater, it can play a role in its vertical stratification. Increasing … 展开
In the midlatitudes, an excess of evaporation over precipitation leads to surface waters being saltier than deep waters. In such regions, the vertical stratification is due to surface waters being warmer than deep … 展开
• Thermocline – A cline based on difference in water temperature,
• Chemocline – A cline based on difference in water 展开• Underwater diving portal
• Hypersaline lake – Landlocked body of water that contains concentrations of salts greater than the sea
• Isopycnal – Line connecting points of a specific density or potential density 展开CC-BY-SA 许可证中的维基百科文本 Halocline | Salinity Gradient, Temperature Variation & Stratification ...
What Is Halocline? - American Oceans
The Halocline - Dive & Discover
The halocline sits on top of the very salty water in the basin and touches the sides of the basin. Researchers call that area the “bathtub ring” because it is like the ring of soap scum and dirt that forms on a bathtub when the water is …
The Arctic Ocean halocline and its interannual ... - ScienceDirect
Halocline - an overview | ScienceDirect Topics
Halocline - SpringerLink
Halocline - (Oceanography) - Vocab, Definition, Explanations
Arctic Ocean stratification set by sea level and freshwater inputs ...
The Western Eurasian Basin Halocline in 2017: Insights …
2020年6月23日 · The halocline, a layer near the surface where salinity increases rapidly with depth, isolates sea ice from the heat stored in the salty Atlantic water below. Waters in the halocline could be traced back to two different sources: …
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