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- Ocean_current abstract "An ocean current is a continuous, directed movement of seawater generated by the forces acting upon this mean flow, such as breaking waves, wind, Coriolis effect, cabbeling, temperature and salinity differences, with tides caused by the gravitational pull of the Moon and the Sun. Depth contours, shoreline configurations and interaction with other currents influence a current's direction and strength. A deep current is any ocean current at a depth of greater than 100m. A part of oceanography is the science studying ocean currents.Ocean currents can flow for great distances, and together they create the great flow of the global conveyor belt which plays a dominant part in determining the climate of many of the Earth’s regions. Perhaps the most striking example is the Gulf Stream, which makes northwest Europe much more temperate than any other region at the same latitude. Another example is Lima, Peru where the climate is cooler (sub-tropical) than the tropical latitudes in which the area is located, due to the effect of the Humboldt Current.".
- Ocean_current thumbnail Corrientes-oceanicas.gif?width=300.
- Ocean_current wikiPageExternalLink oceancurrents.rsmas.miami.edu.
- Ocean_current wikiPageExternalLink oceanmotion.org.
- Ocean_current wikiPageExternalLink oscar.htm.
- Ocean_current wikiPageExternalLink www.cocmp.org.
- Ocean_current wikiPageExternalLink english.
- Ocean_current wikiPageExternalLink facts.
- Ocean_current wikiPageExternalLink www.oscar.noaa.gov.
- Ocean_current wikiPageID "376476".
- Ocean_current wikiPageRevisionID "605998178".
- Ocean_current hasPhotoCollection Ocean_current.
- Ocean_current subject Category:Ocean_currents.
- Ocean_current subject Category:Oceans.
- Ocean_current subject Category:Physical_oceanography.
- Ocean_current comment "An ocean current is a continuous, directed movement of seawater generated by the forces acting upon this mean flow, such as breaking waves, wind, Coriolis effect, cabbeling, temperature and salinity differences, with tides caused by the gravitational pull of the Moon and the Sun. Depth contours, shoreline configurations and interaction with other currents influence a current's direction and strength. A deep current is any ocean current at a depth of greater than 100m.".
- Ocean_current label "Corrente oceanica".
- Ocean_current label "Corrente oceânica".
- Ocean_current label "Corriente marina".
- Ocean_current label "Courant marin".
- Ocean_current label "Meeresströmung".
- Ocean_current label "Ocean current".
- Ocean_current label "Prąd morski".
- Ocean_current label "Zeestroom".
- Ocean_current label "Морские течения".
- Ocean_current label "تيار محيطي".
- Ocean_current label "洋流".
- Ocean_current label "海流".
- Ocean_current sameAs Mořský_proud.
- Ocean_current sameAs Meeresströmung.
- Ocean_current sameAs Corriente_marina.
- Ocean_current sameAs Itsaslaster.
- Ocean_current sameAs Courant_marin.
- Ocean_current sameAs Arus_air_laut.
- Ocean_current sameAs Corrente_oceanica.
- Ocean_current sameAs 海流.
- Ocean_current sameAs 해류.
- Ocean_current sameAs Zeestroom.
- Ocean_current sameAs Prąd_morski.
- Ocean_current sameAs Corrente_oceânica.
- Ocean_current sameAs m.0211p2.
- Ocean_current sameAs Q129558.
- Ocean_current sameAs Q129558.
- Ocean_current wasDerivedFrom Ocean_current?oldid=605998178.
- Ocean_current depiction Corrientes-oceanicas.gif.
- Ocean_current isPrimaryTopicOf Ocean_current.