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Jason Naylor Department of Atmospheric Sciences, University of North Dakota, Grand Forks, North Dakota

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Matthew S. Gilmore Department of Atmospheric Sciences, University of North Dakota, Grand Forks, North Dakota

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Corresponding author address: Jason Naylor, NorthWest Research Associates, 3380 Mitchell Lane, Boulder, CO 80301. E-mail: jnaylor@nwra.com

Corresponding author address: Jason Naylor, NorthWest Research Associates, 3380 Mitchell Lane, Boulder, CO 80301. E-mail: jnaylor@nwra.com

The caption for Fig. 9 in Naylor and Gilmore (2014) incorrectly identifies the symbols in the figure. The figure with its correct caption is presented below. We regret any inconvenience this error may have caused.

Fig. 9.
Fig. 9.

Maximum and minimum perturbations of θep for the TOR (circles) and NON (crosses) simulations. Perturbations are relative to the surface value in the base-state environment. The calculation was performed over a 1 km × 1 km box centered on the circulation at the time of tornadogenesis or tornadogenesis failure.

Citation: Journal of the Atmospheric Sciences 71, 9; 10.1175/JAS-D-14-0204.1

Acknowledgments

The authors thank Dr. Paul Markowski for bringing this error to their attention.

REFERENCE

Naylor, J., and M. S. Gilmore, 2014: Vorticity evolution leading to tornadogenesis and tornadogenesis failure in simulated supercells. J. Atmos. Sci., 71, 12011217, doi:10.1175/JAS-D-13-0219.1.

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  • Naylor, J., and M. S. Gilmore, 2014: Vorticity evolution leading to tornadogenesis and tornadogenesis failure in simulated supercells. J. Atmos. Sci., 71, 12011217, doi:10.1175/JAS-D-13-0219.1.

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  • Fig. 9.

    Maximum and minimum perturbations of θep for the TOR (circles) and NON (crosses) simulations. Perturbations are relative to the surface value in the base-state environment. The calculation was performed over a 1 km × 1 km box centered on the circulation at the time of tornadogenesis or tornadogenesis failure.

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