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- Halothermal_circulation abstract "The term halothermal circulation refers to the part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and evaporation.The adjective halothermal derives from halo- referring to salt content and -thermal referring to temperature, factors which together determine the density of sea water. Halothermal circulation is driven primarily by salinity changes and secondarily by temperature changes (as opposed to the thermohaline mode in modern oceans). The generation of high salinity surface waters at low latitudes, which were therefore of higher density and thus sank, is thought to have been the dominant ocean circulation driver during greenhouse climates such as the Cretaceous. Similar dynamics operate today in the Mediterranean.The formation of bottom waters by halothermal dynamics is considered to be one to two orders of magnitude weaker than in thermohaline systems.".
- Halothermal_circulation wikiPageID "22784944".
- Halothermal_circulation wikiPageLength "1448".
- Halothermal_circulation wikiPageOutDegree "10".
- Halothermal_circulation wikiPageRevisionID "610816428".
- Halothermal_circulation wikiPageWikiLink Category:Geological_processes.
- Halothermal_circulation wikiPageWikiLink Category:Physical_oceanography.
- Halothermal_circulation wikiPageWikiLink Cretaceous.
- Halothermal_circulation wikiPageWikiLink Density_gradient.
- Halothermal_circulation wikiPageWikiLink Greenhouse_and_icehouse_Earth.
- Halothermal_circulation wikiPageWikiLink Mediterranean_Sea.
- Halothermal_circulation wikiPageWikiLink Properties_of_water.
- Halothermal_circulation wikiPageWikiLink Salinity.
- Halothermal_circulation wikiPageWikiLink Thermohaline_circulation.
- Halothermal_circulation wikiPageWikiLink Wikt:thermo-.
- Halothermal_circulation wikiPageWikiLinkText "Halothermal circulation".
- Halothermal_circulation wikiPageWikiLinkText "halothermal dynamics".
- Halothermal_circulation wikiPageUsesTemplate Template:Ocean-stub.
- Halothermal_circulation wikiPageUsesTemplate Template:Physical_oceanography.
- Halothermal_circulation subject Category:Geological_processes.
- Halothermal_circulation subject Category:Physical_oceanography.
- Halothermal_circulation type Process.
- Halothermal_circulation comment "The term halothermal circulation refers to the part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and evaporation.The adjective halothermal derives from halo- referring to salt content and -thermal referring to temperature, factors which together determine the density of sea water. Halothermal circulation is driven primarily by salinity changes and secondarily by temperature changes (as opposed to the thermohaline mode in modern oceans).".
- Halothermal_circulation label "Halothermal circulation".
- Halothermal_circulation sameAs Q5643468.
- Halothermal_circulation sameAs m.05zhw99.
- Halothermal_circulation sameAs Q5643468.
- Halothermal_circulation wasDerivedFrom Halothermal_circulation?oldid=610816428.
- Halothermal_circulation isPrimaryTopicOf Halothermal_circulation.