Fig. 8: Change in the mean state of low-level zonal wind under global warming in CMIP6.
From: Enhanced impact of the Aleutian Low on increasing the Central Pacific ENSO in recent decades
Differences in the background mean spring 850-hPa zonal wind between present-day climate period (historical simulations over 1920–1999) and future climate period (SSP-585 simulations over 2020–2099) for 34 CMIP6 models (Supplementary Table 2) and their MME. Stippling regions indicate the differences that are significantly different from zero at the 95% confidence level.
