Correction to: The role of transient eddies and diabatic heating in the maintenance of European heat waves: a nonlinear quasi-stationary wave perspective

1 Correction to: Climate Dynamics https://doi.org/10.1007/s00382-021-05628-9

In the original version of the article, there is a diagonal line in Figs. 2 and 8. The correct Fig. 2 and Fig. 8 is given below,

Fig. 2

a Composite spatial pattern of temperature anomalies $T_{ano}$ (shading) and the heat wave magnitude HWMId (contour); the green dashed box depicts the used European region of our study. b The corresponding composites of the 200 hPa streamfunction anomaly; contour interval is $1 \times 10^6\,\,\mathrm{{m}}^2\,\mathrm{{s}}^{-1}$. Probability density functions of daily Europe $T_{ano}$ versus NAO c, NINO3.4 d and IOD e index for JJA (blue) and the heat wave events stated in Table 1 (red)

Fig. 8

Same as Fig. 7b, but now the transient vorticity flux is decomposed into different nonlinear interaction parts stemming from different frequency ranges: a $-\nabla \cdot \overline{({\mathbf {v}}_L^\prime \zeta _L^\prime )}$, b $-\nabla \cdot \overline{({\mathbf {v}}_L^\prime \zeta _H^\prime )}$, c $-\nabla \cdot \overline{({\mathbf {v}}_H^\prime \zeta _L^\prime )}$, and d $-\nabla \cdot \overline{({\mathbf {v}}_H^\prime \zeta _H^\prime )}$

The original article has been corrected.