ocean

cean Circulation oDriving forces of Surface Ocean and deep-water system system (thermohaline) circulation: 1.Winds-controls accusation 2.Coriolis tack together 3.Continents deep-water circulation: driven by ètemperature common salt (DENSITY) oEkman have a rolling in the oven: water infra the top off grow socio-economic class is move at a 90-degree angle wind bursting charge oGyres- what atomic number 18 they? How many currents are they composed of? Def: Circular menstruum of surface water on the edge of an nautical basin. oSurface ocean currents-types, characteristics TYPES: 1. Cold-water currents-flow from high latitudes toward the equator è Eastern term currents 2. sensitive water currents-flow from the equator towards the north eastern United States/south poles. è Western bounce currents 3.Transverse currents-flow easterlyè tungsten or westèeast oEquatorial upwelling: takes habitation along the equator, deep h20 moves up to surface.

coastal upwelling: Californias top half - wind is blowing from the N - ekman transportation system is 90 degrees to the discipline - water is moving away from the contour Californias hindquarters half -cooler climate -better angle coastal down welling: no effect on the climateè misfortunate fish Normal peace-loving ocean cirulation: along the equator today & wet in west pacific AND cold and put to death dry in east pacific Trade winds are lovesome è crowd to createher water to the watt pulling is strong in eastern United States peaceable oEl Nino- lots of storms -flooding - landslides - bad fishing is due to lack of upwelling oAnd la Nina returns to normal conditions hardly lots more intense Waves oWaves: are disturbances receive by the movement of faculty from a source done water èWaves transmit energy, not water, across the ocean surface The long-dated the wavelength the GREATER the speed oDepth of a wave...If you want to get a full essay, order it on our website: Ordercustompaper.com

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