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• W2089216077 abstract "An analysis is made of 11 Great Plains nocturnal thunderstorm occurrences that have no obvious synoptic scale support. The pressure patterns and local terrain configurations are input to a numerical boundary-layer model that computes the vertically integrated boundary-layer convergence. The time and space phasing of the vertical velocities thus obtained are in good agreement with the time and space phasing of all 11 thunderstorm occurrences for the beginning of the activity, but they are acceptable in only 6 cases for the termination of the activity. There is a tendency for the model to forecast boundary-layer convergence where no thunderstorms occur; but in many such cases, stability and humidity data are unfavorable for thunderstorm activity." @default.
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• W2089216077 date "1973-12-01" @default.
• W2089216077 modified "2023-10-14" @default.
• W2089216077 title "Correlation of Nocturnal Thunderstorms and Boundary-Layer Convergence" @default.
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• W2089216077 doi "https://doi.org/10.1175/1520-0493(1973)101<0877:contab>2.3.co;2" @default.
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