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- Mode_water abstract "Mode water is defined as a particular type of water mass, which is nearly vertically homogeneous. Its vertical homogeneity is caused by the deep vertical convection in winter. The first term to describe this phenomenon is 18° water, which is used by L.V. Worthington to describe the isothermal layer in the northern Sargasso Sea cool to a temperature of about 18 °C each winter. Then Masuzawa introduced the subtropical mode water concept to describe the thick layer of temperature 16–18 °C in the northwestern North Pacific subtropical gyre, on the southern side of the Kuroshio Extension. The terminology mode water was extended to the thick near-surface layer north of the Subantarctic Front by McCartney, who identified and mapped the properties of the Subantarctic mode water (SAMW). After that, McCartney and Talley then applied the term subpolar mode water (SPMW) to the thick near-surface mixed layers in the North Atlantic’s subpolar gyre.".
- Mode_water thumbnail Antarctic_bottom_water.svg?width=300.
- Mode_water wikiPageID "40984195".
- Mode_water wikiPageLength "6450".
- Mode_water wikiPageOutDegree "22".
- Mode_water wikiPageRevisionID "671324508".
- Mode_water wikiPageWikiLink Baroclinity.
- Mode_water wikiPageWikiLink Biological_pump.
- Mode_water wikiPageWikiLink Brunt–Väisälä_frequency.
- Mode_water wikiPageWikiLink Buoyancy.
- Mode_water wikiPageWikiLink Carbon_dioxide.
- Mode_water wikiPageWikiLink Category:Oceanography.
- Mode_water wikiPageWikiLink Convection.
- Mode_water wikiPageWikiLink Isothermal_process.
- Mode_water wikiPageWikiLink Kuroshio_Current.
- Mode_water wikiPageWikiLink Mixed_layer.
- Mode_water wikiPageWikiLink Photic_zone.
- Mode_water wikiPageWikiLink Potential_density.
- Mode_water wikiPageWikiLink Potential_vorticity.
- Mode_water wikiPageWikiLink Salinity.
- Mode_water wikiPageWikiLink Sargasso_Sea.
- Mode_water wikiPageWikiLink Subantarctic_Mode_Water.
- Mode_water wikiPageWikiLink Subduction.
- Mode_water wikiPageWikiLink Turbulence.
- Mode_water wikiPageWikiLink Water_mass.
- Mode_water wikiPageWikiLink File:Antarctic_bottom_water.svg.
- Mode_water wikiPageWikiLink File:Mode_water_chao_sun.tif.
- Mode_water wikiPageWikiLink File:Mode_water_chao_sun1.tif.
- Mode_water wikiPageWikiLinkText "mode water".
- Mode_water wikiPageUsesTemplate Template:Reflist.
- Mode_water subject Category:Oceanography.
- Mode_water comment "Mode water is defined as a particular type of water mass, which is nearly vertically homogeneous. Its vertical homogeneity is caused by the deep vertical convection in winter. The first term to describe this phenomenon is 18° water, which is used by L.V. Worthington to describe the isothermal layer in the northern Sargasso Sea cool to a temperature of about 18 °C each winter.".
- Mode_water label "Mode water".
- Mode_water sameAs Q17147710.
- Mode_water sameAs m.0yx_bwy.
- Mode_water sameAs Q17147710.
- Mode_water wasDerivedFrom Mode_water?oldid=671324508.
- Mode_water depiction Antarctic_bottom_water.svg.
- Mode_water isPrimaryTopicOf Mode_water.