Amplified warming over western highlands is carried downstream by westerlies, strengthening low-level inversions and thereby raising the maxima of moist heat and convection extremes in the midlatitudes.
S1), the midlat- itude mean biases are relatively small in the selected models but substantially larger, especially for CAPE𝑐, in the remaining five models (Supplementary Fig
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Future Amplification of Moist Weather Extremes in the Midlatitudes
Amplified warming over western highlands is carried downstream by westerlies, strengthening low-level inversions and thereby raising the maxima of moist heat and convection extremes in the midlatitudes.