Fig. 3: Response of cloud ice in IWP percentile and temperature space in the GSRM experiments. | npj Climate and Atmospheric Science

Fig. 3: Response of cloud ice in IWP percentile and temperature space in the GSRM experiments.

From: Kilometer-scale global warming simulations and active sensors reveal changes in tropical deep convection

Fig. 3

Fractional increase per TS warming of ice mixing ratio at fixed temperature and fixed IWP percentile in (a) the +4K experiment and (b) the global warming experiment. The white dashed line shows the 7 % K−1 isoline where the increase in ice mixing ratio approximately corresponds to the increase in boundary layer specific humidity. The IWP response from Fig. 2 is reproduced in the upper panel of a, b.

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