#GlobalMeanSurfaceTemperature

AI4PEXAi4pex
2024-07-16

Three particular responses of the are critically important for our understanding of , but remain highly uncertain:

(I) The change in for a doubling of atmospheric , which determines the long-term warming of the Earth.
(II) The rate at which excess heat is sequestered into the deep ocean.
(III) The fraction of that remains in the atmosphere, which is controlled by the efficacy of ocean and terrestrial .

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