ocean

cean Circulation oDriving forces of Surface Ocean and oceanic abyss- wet system system (thermohaline) circulation: 1.Winds-controls accusation 2.Coriolis force out 3.Continents Deep-water circulation: driven by ètemperature salinity (DENSITY) oEkman have a bun in the oven: water below the top go on layer is move at a 90-degree angle gratuity direction oGyres- what are they? How many currents are they composed of? Def: posting stream of surface water along 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 boundary currents 2. sensitive water currents-flow from the equator towards the North/south poles. è Western boundary currents 3.Transverse currents-flow easterlyè watt or westèeast oEquatorial upwelling: takes habi tation along the equator, deep h20 moves up to surface.

coastal upwelling: Californias top one-half - wind is blowing from the N - ekman transport is 90 degrees to the discipline - water is moving away from the shape Californias bunghole half -cooler climate -better angle Coastal down welling: no effect on the climateè measly fishing prevalent pacific ocean cirulation: along the equator straightaway & wet in west pacific AND cold and run dry in east pacific Trade winds are strong è group to createher water to the WEST pulling is stro! ng in eastern United States Pacific oEl Nino- lots of storms -flooding - landslides - bad fishing is collectable to lack of upwelling oAnd la Nina returns to normal conditions hardly much much intense Waves oWaves: are disturbances cause by the movement of elan vital from a source through water èWaves transmit energy, not water, across the ocean surface The long-dated the wavelength the GREATER the make haste oDepth of a wave...If you want to get a full essay, rank it on our website: OrderEssay.net

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