cold ocean current on the movement of ice bridge
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Melting sea ice could change globalocean circulation. In the far North Atlantic Ocean, surface waters cooland sink, forming deep water. This sinking helps drive the “global conveyor belt,” the ocean currents that move warm water from the tropics toward the poles.
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sea streams asume a noteworthy part in in the convayence of warthm supplement,water salt far and widethe dampness of local get infiuenced byby an adjusment in the sea stream
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