There were errors in the units for the variance spectra in the legend of Fig. 4 and in the y-axis labels of Figs. 5a, 7, 14b, and 14c in Zhou et al. (2018). These errors did not affect any discussion or conclusions of the study. The corrected figures (Figs. 4, 5, 7, and 14) are shown below.

Fig. 4.

Variance spectra of total water mixing ratio at 700 m, LWP, pseudoalbedo, and optical depth for simulation Nd10 at 10 h multiplied by the wavenumber k.

Fig. 4.

Variance spectra of total water mixing ratio at 700 m, LWP, pseudoalbedo, and optical depth for simulation Nd10 at 10 h multiplied by the wavenumber k.

Fig. 5.

(a) Variance spectra of total water mixing ratio at 700 m at 10 h multiplied by the wavenumber k and (b) temporal evolution of total water mixing ratio variance length scale (defined in Zhou et al. 2018) at 700 m for Nd10, Nd35, and Nd65. Simulations as in Fig. 2 of Zhou et al. (2018).

Fig. 5.

(a) Variance spectra of total water mixing ratio at 700 m at 10 h multiplied by the wavenumber k and (b) temporal evolution of total water mixing ratio variance length scale (defined in Zhou et al. 2018) at 700 m for Nd10, Nd35, and Nd65. Simulations as in Fig. 2 of Zhou et al. (2018).

Fig. 7.

Variance spectra of total water mixing ratio of (a) Nd10 at different levels at 10 h, (b) Nd10 at 700 m at three times, and (c) Nd65 at 700 m at three times.

Fig. 7.

Variance spectra of total water mixing ratio of (a) Nd10 at different levels at 10 h, (b) Nd10 at 700 m at three times, and (c) Nd65 at 700 m at three times.

Fig. 14.

(a) Spectral decomposition of the production term in Eq. (1) of Zhou et al. (2018), (b) variance spectra of vertical wind velocity, and (c) variance spectra of total water mixing ratio at altitude 700 m and time 10 h. Setup of simulations as indicated in legend and as described in main text and summarized in Table 1 of Zhou et al. (2018).

Fig. 14.

(a) Spectral decomposition of the production term in Eq. (1) of Zhou et al. (2018), (b) variance spectra of vertical wind velocity, and (c) variance spectra of total water mixing ratio at altitude 700 m and time 10 h. Setup of simulations as indicated in legend and as described in main text and summarized in Table 1 of Zhou et al. (2018).

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