Similarly as Earth's turn makes the overall breezes, it makes surface flows inside the seas. Affe exchange winds, surface waters close to the equator stream from east to west. As in the clima Coriolis power makes water be redirected away from the equator (toward the north in the No Hemisphere, toward the south in the Southern Hemisphere). This Coriolis Effect sets up a rota convection inside the seas, and flows commonly stream in a clockwise revolution in the North Hemisphere and a counter-clockwise way in the Southern Hemisphere. As it arrives at the pos water cools and sinks. Winning breezes in northern and southern scopes help to make cold-wa surface flows that stream back toward the equator along the west bank of landmasses