Articles | Volume 10, issue 1
Earth Syst. Sci. Data, 10, 317–324, 2018
https://doi.org/10.5194/essd-10-317-2018
Earth Syst. Sci. Data, 10, 317–324, 2018
https://doi.org/10.5194/essd-10-317-2018

  21 Feb 2018

21 Feb 2018

Surface and top-of-atmosphere radiative feedback kernels for CESM-CAM5

Angeline G. Pendergrass et al.

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Cited articles

Block, K. and Mauritsen, T.: Forcing and feedback in the MPI-ESM-LR coupled model under abruptly quadrupled CO2, J. Adv. Model. Earth Syst., 5, 676–691, https://doi.org/10.1002/jame.20041, 2013. 
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Feldl, N. and Roe, G. H.: The nonlinear and nonlocal nature of climate feedbacks, J. Climate, 26, 8289–8304, https://doi.org/10.1175/JCLI-D-12-00631.1, 2013. 
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We document and validate radiative kernels for the surface and top-of-atmosphere calculated with NCAR's CESM1 climate model. A radiative kernel is the change in radiation in response to a small change in a property of the atmosphere or surface, essentially a partial derivative. They are used to quantify temperature, water vapor, surface albedo, and cloud feedbacks. We made these kernels because few are available for the surface. We also validate the kernels against the expected model responses.