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Figure D: The additional carbon dioxide being absorbed by the oceans impact the ocean circulations and currents that drive weather, temperature, precipitation, and seasons. 1Climate Institute. Oceans and sea level rise: Consequences of climate change on the oceans, thermohaline circulation.
For most of this time the water remains in the colder deep regions of the thermohaline conveyor belt because there the flow rate is slow, at around one to three kiloÂ­metres per day, due to its high density. The amount of water involved in this cycle is truly immense.