Time Scales of Climate Response

@inproceedings{Stouffer2004TimeSO,
  title={Time Scales of Climate Response},
  author={Ronald J. Stouffer and Ronald. Stouffer},
  year={2004}
}
A coupled atmosphere–ocean general circulation model (AOGCM) is integrated to a near-equilibrium state with the normal, half-normal, and twice-normal amounts of carbon dioxide in the atmosphere. Most of the ocean below the surface layers achieves 70% of the total response almost twice as fast when the changes in radiative forcing are cooling as compared to the case when they are warming the climate system. In the cooling case, the time to achieve 70% of the equilibrium response in the… CONTINUE READING
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