Fig. 3: Zonal mean response.
From: Robust but weak winter atmospheric circulation response to future Arctic sea ice loss
Latitude-height cross sections of the multi-model ensemble mean zonally averaged DJF response of a temperature (\(\bar{T}\), colours, K, where the overbar denotes the zonal average) and transformed Eulerian mean (TEM, Methods) circulation (arrows), b zonal wind (\(\bar{u}\), ms−1), and c upward Eliassen-Palm (EP) flux (Fp, colours, standard deviations) and EP flux vectors (arrows representing Fϕ and Fp), d divergence of northward EP flux (∇ϕFϕ, standard deviations). Stippling as in Fig. 1. To aid visualisation the TEM circulation and EP fluxes are standardised by dividing by the internal variability of the present-day simulations (Methods).
