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Dale R. Durran University of Washington, Seattle, Washington

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Peter N. Blossey University of Washington, Seattle, Washington

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Corresponding author address: Dale R. Durran, University of Washington, Atmospheric Sciences, Box 351640, Seattle, WA 98195-1640. E-mail: drdee@uw.edu

Corresponding author address: Dale R. Durran, University of Washington, Atmospheric Sciences, Box 351640, Seattle, WA 98195-1640. E-mail: drdee@uw.edu

In Table 3 of Durran and Blossey (2012), the values of Lx, Lz, and ψ0 for the nonhydrostatic case were in error. The table has been reproduced in its entirety here with the correct values.

Table 3.

Physical and numerical parameters for the nonlinear simulations.

Table 3.

In addition, the bottom panel of Fig. 9 showed the results of a simulation using different parameter values than those in the table. The correct figure is shown below.

Fig. 9.
Fig. 9.

Contours of the horizontal velocity at t = td in the central portion of the domain for (a) case NH and (b) case H. Gray shades show contours of ψ with steps in the grayscale at ±5 and ±15 m2 s−2 in case NH and ±1 m2 s−2 in case H.

Citation: Monthly Weather Review 141, 8; 10.1175/MWR-D-12-00344.1

Last, the discussion of gravity wave frequencies for the case where occurs on p. 410 of Durran (2010), rather than p. 412 as indicated on p. 1316 of Durran and Blossey (2012).

Acknowledgments

The authors regret any confusion that these errors may have caused. They would like to thank Oswald Knoth and Hilary Weller for alerting them to the presence of the errors.

REFERENCES

  • Durran, D. R., 2010: Numerical Methods for Fluid Dynamics: With Applications in Geophysics. Springer, 516 pp.

  • Durran, D. R., and P. N. Blossey, 2012: Implicit–explicit multistep methods for fast-wave–slow-wave problems. Mon. Wea. Rev., 140, 13071325.

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  • Durran, D. R., 2010: Numerical Methods for Fluid Dynamics: With Applications in Geophysics. Springer, 516 pp.

  • Durran, D. R., and P. N. Blossey, 2012: Implicit–explicit multistep methods for fast-wave–slow-wave problems. Mon. Wea. Rev., 140, 13071325.

    • Search Google Scholar
    • Export Citation
  • Fig. 9.

    Contours of the horizontal velocity at t = td in the central portion of the domain for (a) case NH and (b) case H. Gray shades show contours of ψ with steps in the grayscale at ±5 and ±15 m2 s−2 in case NH and ±1 m2 s−2 in case H.

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