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O. Geoffroy, D. Saint-Martin and A. Ribes Quantifying the sources of spread in climate change experiments Geophysical Research Letters 39

Version of Record online: 21 DEC 2012 | DOI: 10.1029/2012GL054172

Key Points

  • The total radiative feedback is the main contributor to the inter-model spread
  • The adjusted radiative forcing is also an important source of spread of the TCR
  • The role of the efficacy of deep-ocean heat uptake is found to be not negligible

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