Anton L. Hales – författare
Visar alla böcker från författaren . Handla med fri frakt och snabb leverans.
2 produkter
2 produkter
E-bok
PDF, Engelska, 1979317 kr
Läs direkt efter köp
An Introduction to Dynamic Meteorology, Second Edition deals with rapid advances in the science of dynamic meteorology. This book presents dynamic meteorology as a cohesive subject with a central unifying body of theory, namely, the quasi-geostrophic system. Topics range from the basic conservation laws to circulation and vorticity, planetary boundary layer, synoptic scale motions in middle latitudes, atmospheric oscillations, midlatitude synoptic systems, dynamics of the stratosphere, and tropical motions. This volume is comprised of 12 chapters and begins with a discussion on the fundamental fluid dynamics necessary for understanding large-scale atmospheric motions, including expanded treatments of atmospheric thermodynamics and of the planetary boundary layer. The reader is then introduced to the basics of modern dynamical meteorology, including the stratospheric dynamics. The energetics of the lower stratosphere, vertically propagating planetary waves, the quasi-biennial oscillation, and the ozone layer are considered. The final chapter reviews the dynamics of the tropical atmosphere, with emphasis on large-scale motions in the equatorial zone, the origin of equatorial disturbances, and tropical cyclones. A number of additional problems that span a wide range in difficulty are included, and answers to selected problems are provided. Throughout the book, the emphasis is on physical principles rather than mathematical elegance. Some use is made of vector calculus. This book is a valuable resource for meteorologists and those working in the field of atmospheric sciences.
E-bok
PDF, Engelska, 20161 015 kr
Läs direkt efter köp
Energy at the Surface of the Earth: An Introduction to the Energetics of Ecosystems presents way of looking at the manner in which the biological, physical, and cultural systems that mantle the landmasses of our planet receive, transform, and give off energy, which is an essential condition of existence that takes many forms. Energy conversions establish the climate in which these systems operate. The principal forms of energy that are converted at the ecosystem scale include radiant, latent, mechanical, chemical and fossil, and thermal. The book begins with radiant energy absorbed by ecosystems—a phenomenon that is independent of their surface temperature and that can be looked on as a burden or a gift, depending on circumstances. An increase in such absorption raises surface temperature, as described in the fulcrum chapter of the book, Chapter VIII. This increase in turn sets into action outflows of energy that by the first law of thermodynamics are equal in energy units, although not necessarily equal in quality to the inflows. The final chapters deal with vertical stratification and areal contrasts in energy budgets, the augmented energy budget of the city, and the responses that serve to keep the budget balanced.