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Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
The Coriolis Effect is the phenomenon that effects global winds. A convection cell is a form of wind and this is the first part of the coriolis effect.
The geostrophic wind balance is not possible because the Coriolis force vanishes at the Equator.
corolis effect...or..coriolis effect...something with those letters...
Cyclones don't form at the equator. The Coriolis effect is a key element in the formation of cyclones. Its influence is negligible at the equator.
The Coriolis effect.
similarity is currents form gyres. difference is currents are any movement of water in one specific direction and gyres are circular patterns of water
wind.Surface currants form by global winds, Coriolis effect (earth's rotation) and continental deflections (surface currents meet continents they change direction).
its because currents form gyres and the wind is so much that it found a circular patterns
The three factors that help form deep currents are ...density,salinity,and tempature.
wind.Surface currants form by global winds, Coriolis effect (earth's rotation) and continental deflections (surface currents meet continents they change direction).
its because currents form gyres and the wind is so much that it found a circular patterns
Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
i know its the coriolis affect thats all i know
Surface currents are caused by the friction of wind on the water. The currents are also affected by the Coriolis Effect, which is the apparent deflection of objects moving in a straight path relative to the earth's surface.