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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.
Deep ocean currents are driven by density and temperature gradients. Thermohaline circulation is also known as the ocean's conveyor belt (which refers to deep ocean density driven ocean basin currents). These currents, called submarine rivers, flow under the surface of the ocean and are hidden from immediate detection. Where significant vertical movement of ocean currents is observed, this is known as upwelling and downwelling.