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Pages 82-83

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From page 82...
... Conditioning the Air for Overturning A proclivity for overturning is enhanced as the lower atmosphere is warmed. This occurs daily after sunrise, and afternoons are often marked by puffy clouds indicative of rising thermal currents.
From page 83...
... THUNDERSTORM ORIGINS, MORPHOLOGY, AND DYNAMICS FIGURE 7.2 Photograph in visible light from synchronous Meteorological Satellite SMS-1, 6 May 1975, 1405 CST. A major squall line harboring tornadoes lies across the central United States.

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  • lower atmosphere


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