Modeling Swishing Free Throws Michael Loney Advised by Dr. Schmidt Senior Seminar Department of Mathematics and Statistics South Dakota State University.
1. The horizontal equations of motion: smaller-scale motion 2. The vertical equation of motion 3. The thermal wind ATOC 4720 class34.
MesoscaleM. D. Eastin Deep Convection: Physical Processes.
When advection destroys balance, vertical circulations arise COMET-MSC Winter Weather Course 29 Nov. - 10 Dec. 2004 ppt started from one by James T. Moore.
Single Cell Thunderstorms METR 4803 Hazardous Weather Detection and Prediction Spring, 2005 Semester Kelvin K. Droegemeier School of Meteorology University.
