Fig. 8: Impact of emergent constraint.
From: Robust but weak winter atmospheric circulation response to future Arctic sea ice loss
Refractive index (n2) response (standardised) for a the multi-model ensemble mean (EM) and b the ensemble regression (ER). c, d As a, b but for stratospheric zonal wind (ms−1) at 10 hPa. e, f As a, b but for near-surface zonal wind (ms−1) at 925 hPa. Arrows in a and b show the EP flux response (standardised). Colour bars represent each column. Stippling shows where the EM or ER response is significant (95% confidence interval, Methods). All data are for DJF.
