392 pages, Figs
Despite major advances in the observation and numerical simulation of the atmosphere, basic features of the Earth's climate remain poorly understood. Integrating the available data and computational resources to improve our understanding of the global circulation of the atmosphere remains a challenge. Theory must play a critical role in meeting this challenge. This book provides an authoritative summary of the state of the art on this front. Bringing together seventeen of the field's leading experts to address those aspects of the global circulation of the atmosphere most relevant to climate, the book brings the reader up to date on the key frontiers in general circulation theory - including the nonlinear and turbulent global-scale dynamics that determine fundamental aspects of the Earth's climate. It covers both tropical and extratropical dynamics. While emphasizing theory, as expressed through relatively simple mathematical models, it also draws connections to simulations with comprehensive general circulation models. Topics include the dynamics of storm tracks, interactions between wave dynamics and the hydrological cycle, monsoons, tropical-extratropical interactions, and the processes controlling atmospheric humidity. An essential resource for graduate students in atmospheric, ocean, and climate sciences and for researchers seeking an overview of the field, "The Global Circulation of the Atmosphere" sets the standard for future research in a science that stands at a critical juncture.
This edited volume, derived from a three-day conference held in 2004, includes 12 comprehensive chapters covering various aspects of the global circulation. The authors are experts in their respective fields; hence the chapters are very informative. -- S.C. Pryor, Choice [This book] represents an outstanding aggregation of science at the forefront written by leading experts of the field. It is hard to imagine someone reading it without enhancing their insight into the fascinating field of the general circulation of the atmosphere. -- Thomas Birner, Bulletin of the American Meteorological Society
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