to the warming waters of the ocean, they must travel further north to Long Island to search out cool enough waters. The amount of CO2 within the atmosphere, on the rates and mechanisms of CO2 trade between the sea and the air, and the fluctuations in marine organic carbon have been studied since shortly after the start of the Industrial Revolution. Since 1990, there was a major lower in the strength of the CO2 sink, which is as a result of increase of partial stress of ocean floor CO2 attributable to evaporation and the accompanying focus of solutes in the water.
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