Correction to “Nonlinearity of the combined warm ENSO and QBO effects on the Northern Hemisphere polar vortex in MAECHAM5 simulations”

Abstract

Figure 3. Vertical profiles for the ENW–CTW (black) and ENE–CTE (gray) ensemble differences of the vertical (dashed) and meridional (dashed-dotted) components of the EP flux averaged from 60 N to 80 N and the Eliassen Palm (EP) flux divergence (solid) averaged from 50 N to 80 N. Values plotted are 10 Fy (N m ), 10 Fz (N m ), and 0.5 div(EP) in m s 1 d . JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, D20117, doi:10.1029/2009JD013257, 2009