On land, elevated CO2 and an extended rising season have stimulated plant development. Climate change will increase droughts and warmth waves that inhibit plant growth, which makes it unsure whether this carbon sink will continue to develop sooner or later. As more CO2 and warmth are absorbed by the ocean, it acidifies, its circulation modifications and phytoplankton takes up much less carbon, decreasing the rate at which the ocean absorbs atmospheric carbon.
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