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Excerpt from Frontal Motion in the Atmosphere Various initial and boundary conditions are considered, and a comparison of their effect on the occlusion process is made. In all cases, the cold front propagates faster than the warm front, and a relatively strong mass convergence flow exists behind the cold front only. A cyclonic circulation pattern also appears near the cold front. These facts suggest the occurrence of severe storms associated with cold fronts, but not with warm fronts in the atmosphere. The methods developed here have application to general free boundary problems in fluid dynamics. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.

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