Extended Data Fig. 2: Differences in clear-sky radiative heating rate between CNTL and MD1 aqua-planet simulations. | Nature Geoscience

Extended Data Fig. 2: Differences in clear-sky radiative heating rate between CNTL and MD1 aqua-planet simulations.

From: Substantial influence of vapour buoyancy on tropospheric air temperature and subtropical cloud

Extended Data Fig. 2

(a) Total clear-sky radiative heating rate response (K/day). (b) Partial clear-sky radiative heating rate response due to changes in temperature (K/day). (c) Partial clear-sky radiative heating rate response due to changes in specific humidity (K/day). (d) Sum of (b) and (c).

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