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maximum intensityin use at National Severe Storms Laboratory. 8.Size distribution of graupel and hail. 325.SMITH, ARTHUR H., JR.:SMITH, D. L.:Picture of month-turbulent region. 408.and W. A. Schulz. Weather note-powerline breaks-potentialaid in tornado identification and tracking. 307.SMITH, W. L.:and P. Krishna Rao and R. Koffler. Global sea-surface tempera-ture distribution determined from environmental satellite. 10.and Russell J. Younkin. Operationally useful relationship be-SMITH, WARRENtween

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Joseph B. Olson, Brian A. Colle, Nicholas A. Bond, and Nathaniel Winstead

significantly different from the 4-km nest, so the 1.33-km results are not highlighted in this paper. Each model domain was run simultaneously using one-way nesting, so that the impact of different model resolutions can be quantified. Thirty-two model sigma levels were applied, with 15 levels below 700 hPa in order to better resolve the boundary layer processes. A 10′ and 1′ land-use and topography dataset was utilized in the 36- and 12-km domains, respectively, while the 4-km domain used a 30″ topography

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