CORRIGENDUM

Mario Marcello Miglietta Institute of Atmospheric Sciences and Climate (ISAC), Italian National Research Council (CNR), Lecce/Padua, Italy

Search for other papers by Mario Marcello Miglietta in
Current site
Google Scholar
PubMed
Close
and
Richard Rotunno NCAR,* Boulder, Colorado

Search for other papers by Richard Rotunno in
Current site
Google Scholar
PubMed
Close
Full access

Corresponding author address: Mario Marcello Miglietta, CNRISAC, Strada Provinciale Lecce-Monteroni, Km 1.200, 73100 Lecce, Italy. Email: m.miglietta@isac.cnr.it

Corresponding author address: Mario Marcello Miglietta, CNRISAC, Strada Provinciale Lecce-Monteroni, Km 1.200, 73100 Lecce, Italy. Email: m.miglietta@isac.cnr.it

Incorrect versions of Figs. 5 and 9 were published in Miglietta and Rotunno (2009). The correct figures are shown below.

The authors regret any inconvenience this error may have caused.

REFERENCE

Miglietta, M. M., and R. Rotunno, 2009: Numerical simulations of conditionally unstable flows over a mountain ridge. J. Atmos. Sci., 66 , 18651885.

  • Search Google Scholar
  • Export Citation

Fig. 5.
Fig. 5.

Vertical cross sections (extending from the ground up to 10 km) of the y average of potential temperature perturbation (dark shaded areas), cloud water plus ice content (light shaded areas), rainwater content (contour line for 0.2 × 10−3 kg kg−1), and wind speed (arrows) for the experiments shown in Fig. 3. The results are shown (a) after t = 5 h and (b),(c) at the final integration time t = 10 h.

Citation: Journal of the Atmospheric Sciences 66, 12; 10.1175/2009JAS3304.1

Fig. 9.
Fig. 9.

As in Fig. 5, but for experiments with a = 30 km and (a) U = 2.5 m s−1 and hm = 500 m and (b) U = 10 m s−1 and hm = 2000 m. The two experiments correspond to the same value of hmN/U.

Citation: Journal of the Atmospheric Sciences 66, 12; 10.1175/2009JAS3304.1

* The National Center for Atmospheric Research is sponsored by the National Science Foundation.

Save
  • Miglietta, M. M., and R. Rotunno, 2009: Numerical simulations of conditionally unstable flows over a mountain ridge. J. Atmos. Sci., 66 , 18651885.

    • Search Google Scholar
    • Export Citation
  • Fig. 5.

    Vertical cross sections (extending from the ground up to 10 km) of the y average of potential temperature perturbation (dark shaded areas), cloud water plus ice content (light shaded areas), rainwater content (contour line for 0.2 × 10−3 kg kg−1), and wind speed (arrows) for the experiments shown in Fig. 3. The results are shown (a) after t = 5 h and (b),(c) at the final integration time t = 10 h.

  • Fig. 9.

    As in Fig. 5, but for experiments with a = 30 km and (a) U = 2.5 m s−1 and hm = 500 m and (b) U = 10 m s−1 and hm = 2000 m. The two experiments correspond to the same value of hmN/U.

All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 75 14 0
PDF Downloads 14 7 0