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List of 1700 publications, arranged in geographic units covering the oceanic and inland waters of the northern hemisphere.
Climate modelling is a field in rapid development, and the fltudy of cryospheric processes has become an important part of it. On smaller time scales, the effect of snow cover and sea ice on the atmospheric circulation is of concern for long-range weather forecasting. Thinking in decades or centuries, the effect of a C02 climatic warming on the present-day ice sheets, and the resulting changes in global sea level, has drawn a lot of attention. In particular, the dynamics of marine ice sheets (ice sheets on a bed that would be below sea level after removal of ice and full isostatic rebound) is a subject of continuous research. This interest stems from the fact that the West Antarctic Ice Sheet is a marine ice sheet which, according to some workers, may be close to a complete collapse. The Pleistocene ice ages, or glacial cycles, are best characterized by total ice volume on earth, indicating that on 4 5 large time scales (10 to 10 yr) ice sheets are a dominant component of the climate system. The enormous amount of paleoclimatic information obtained from deep-sea sediments in the last few decades has led to a complete revival of iriterest in the physical aspects of the Pleistocene climatic evolution.
This book provides a detailed review of terminations of ice ages, including a very attractive theory based on dust deposits on ice sheets. While other books on ice ages are mostly short, popular, and non-technical, the only book that attempts to deal with the broad issues of what we know about past ice ages and why they occur is the book by Muller and MacDonald (M&M), published by Praxis. However, despite its many good features, this book suffers from an inordinate emphasis on spectral analysis, a lack of coverage of new data, and a very confusing sequence of chapters. As a result, the data and theory are so intimately entwined that it is difficult to separate one from the other. This volume provides an independent and comprehensive summary of the latest data, theories and analysis. This third edition of what has become the premier reference and sourcebook on ice ages addresses recent topics, and includes new references, new data, and a totally new, greatly expanded treatment of terminations of ice ages.