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Mark T. Stoelinga Department of Atmospheric Sciences, University of Washington, Seattle, Washington

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John D. Locatelli Department of Atmospheric Sciences, University of Washington, Seattle, Washington

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Ralph D. Schwartz Department of Atmospheric Sciences, University of Washington, Seattle, Washington

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Peter V. Hobbs Department of Atmospheric Sciences, University of Washington, Seattle, Washington

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Corresponding author address: Peter V. Hobbs, Dept. of Atmospheric Sciences, University of Washington, Box 351640, Seattle, WA 98195-1640.Email: phobbs@atmos.washington.edu

Corresponding author address: Peter V. Hobbs, Dept. of Atmospheric Sciences, University of Washington, Box 351640, Seattle, WA 98195-1640.Email: phobbs@atmos.washington.edu

In Stoelinga et al. (2003), the descriptions of Figs. 15a and 15b are reversed. The correct caption should reads as follows: Fig. 15. Schematic showing the differences between (a) a warm-sector squall line and (b) a CFA squall line. See text for explanation.

Only the figure caption is in error. The order of the panels themselves, as well as the descriptions of the panels in the text, are correct as published.

REFERENCES

Stoelinga, M. T., J. D. Locatelli, R. D. Schwartz, and P. V. Hobbs, 2003: Is a cold pool necessary for the maintenance of a squall line produced by a cold front aloft? Mon. Wea. Rev., 131 , 95115.

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  • Stoelinga, M. T., J. D. Locatelli, R. D. Schwartz, and P. V. Hobbs, 2003: Is a cold pool necessary for the maintenance of a squall line produced by a cold front aloft? Mon. Wea. Rev., 131 , 95115.

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