OCEAN CURRENTS
current   mass of water moving from one place to another like a river within the ocean
importance: moves drifting organisms from place to place – plankton, disperse young carries eggs and larvae of organisms that have external fertilization brings food, oxygen carries away waste, pollutants
three types of currents surface currents thermohaline circulation (currents) wind-driven vertical currents (upwelling)
surface currents wind driven currents occur at surface horizontal currents caused by friction between wind and water - wind pushes water
surface currents Coriolis effect causes moving objects in northern hemisphere to veer clockwise causes moving objects in southern hemisphere to move counter- clockwise
surface currents Coriolis effect
surface currents gyre massive circular system of wind-driven surface currents cover whole oceans clockwise in Northern hemisphere counter-clockwise in Southern hemisphere
surface currents eddies = warm core rings break off of currents and transport organisms elsewhere
thermohaline circulation (currents) causes deep ocean circulation vertical currents temperature and salinity cause water density differences due to density differences, water masses rise and fall
thermohaline circulation (currents) ↑  salinity = ↑ density  = water mass sinks ↑  temp. = ↓ density = water mass floats
thermohaline circulation (currents)
thermohaline circulation (currents) when combined with surface currents, results in conveyor belt movement of water   around globe
wind driven vertical currents   = upwelling wind blows, moves water away, causes new water to rise up to replace it

Ocean Currents PowerPoint