Titlebook: Atmospheric Convection: Research and Operational Forecasting Aspects; Dario B. Giaiotti,Reinhold Steinacker,Fulvio Stel Book 2007 CISM Udi

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https://doi.org/10.1007/978-3-658-42686-6The conditions necessary for the development of deep moist convection are discussed. This material is followed by an overview of the ways in which convective storms may be organized, with emphasis on the environmental characteristics favoring the various organizational modes.

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Convective Storm Initiation and Organization,The conditions necessary for the development of deep moist convection are discussed. This material is followed by an overview of the ways in which convective storms may be organized, with emphasis on the environmental characteristics favoring the various organizational modes.

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The Concept of Buoyancy and Its Application to Deep Moist Convection,s follows. The quantitative determination of updraft velocity from environmental soundings is complicated by factors such as environmental heterogeneity, hydrometeor loading, freezing, entrainment, and vertical perturbation pressure gradients.

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Thermodynamic Aspects of Topography: the Role of Elevation,on of the surface energy budget in dependence of elevation, the generation of thermally driven slope wind circulations is treated. Finally the differential heating of air in valleys due to the volume reduction is derived and its consequences for valley wind systems. Concluding some concepts of convection over complex terrain are discussed.