• Gregory, J. M., , C. D. Jones, , P. Cadule, , and P. Friedlingstein, 2009: Quantifying carbon cycle feedbacks. J. Climate, 22 , 52325250.

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CORRIGENDUM

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  • 1 Walker Institute for Climate System Research, University of Reading, Reading, and Met Office Hadley Centre, Exeter, United Kingdom
  • | 2 Met Office Hadley Centre, Exeter, United Kingdom
  • | 3 CNRS/IPSL, Paris, and IPSL/LSCE, Gif-sur-Yvette, France
  • | 4 IPSL/LSCE, Gif-sur-Yvette, France, and QUEST, University of Bristol, Bristol, United Kingdom
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* Current affiliation: NCAS-Climate, University of Reading, Reading, and Met Office Hadley Centre, Exeter, United Kingdom

+ Current affiliation: College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom

* Current affiliation: NCAS-Climate, University of Reading, Reading, and Met Office Hadley Centre, Exeter, United Kingdom

+ Current affiliation: College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom

There were some small errors in the caption and body of Table 2 of Gregory et al. (2009), specifically in the lines reporting Eqs. (4) and (18). The corrected table and caption as they should have appeared are shown below.

REFERENCE

Gregory, J. M., , C. D. Jones, , P. Cadule, , and P. Friedlingstein, 2009: Quantifying carbon cycle feedbacks. J. Climate, 22 , 52325250.

Table 2.

Summary of main results for climate and carbon response and feedbacks. References are to equation numbers in the text. The first three groups of formulas apply to equilibrium climate change. The formulas for CO2 emissions apply to time-dependent change in which constant ocean heat uptake efficiency κ is a good approximation.

Table 2.
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