Climate constraint reflects forced signal

Affiliations

¹ Lawrence Livermore National Laboratory, Livermore, CA, USA. pochedley1@llnl.gov.
² Joint Institute for the Study of the Atmosphere and the Ocean, University of Washington, Seattle, WA, USA.
³ Department of Atmospheric Sciences and School of Oceanography, University of Washington, Seattle, WA, USA.
⁴ Lawrence Livermore National Laboratory, Livermore, CA, USA.

Comment

Stephen Po-Chedley et al. Nature. 2018 Nov.

. 2018 Nov;563(7729):E6-E9.

doi: 10.1038/s41586-018-0640-y. Epub 2018 Oct 31.

¹ Lawrence Livermore National Laboratory, Livermore, CA, USA. pochedley1@llnl.gov.
² Joint Institute for the Study of the Atmosphere and the Ocean, University of Washington, Seattle, WA, USA.
³ Department of Atmospheric Sciences and School of Oceanography, University of Washington, Seattle, WA, USA.
⁴ Lawrence Livermore National Laboratory, Livermore, CA, USA.

No abstract available

Comment on

Emergent constraint on equilibrium climate sensitivity from global temperature variability.
Cox PM, Huntingford C, Williamson MS. Cox PM, et al. Nature. 2018 Jan 17;553(7688):319-322. doi: 10.1038/nature25450. Nature. 2018. PMID: 29345639

1. Cox, P. M., Huntingford, C. & Williamson, M. S. Emergent constraint on equilibrium climate sensitivity from global temperature variability. Nature 553, 319–322 (2018). - DOI
1. Leith, C. E. Climate response and fluctuation dissipation. J. Atmos. Sci. 32, 2022–2026 (1975). - DOI
1. Wigley, T. M. L. & Raper, S. C. B. Natural variability of the climate system and detection of the greenhouse effect. Nature 344, 324–327 (1990). - DOI
1. Langen, P. L. & Alexeev, V. A. Estimating 2 × CO₂ warming in an aquaplanet GCM using the fluctuation-dissipation theorem. Geophys. Res. Lett. 32, L23708 (2005). - DOI
1. Schwartz, S. E. Heat capacity, time constant, and sensitivity of Earth’s climate system. J. Geophys. Res. 112, D24S05 (2007). - DOI