The Physics of Glaciers

1. Introduction 2. Transformation of Snow to Ice 3. Grain-Scale Structures and Deformation of Ice 4. Mass Balance Processes: Overview and Regimes 5. Mass Balance Processes: Surface Ablation and Energy Budget 6. Glacial Hydrology 7. Basal Slip 8. The Flow of Ice Masses 9. Temperatures in Ice Masses 10. Large-Scale Structures 11. Reaction of Glaciers to Environmental Changes 12. Glacier Surges 13. Ice Sheets and the Earth System 14. Ice, Sea Level, and Contemporary Climate Change 15. Ice Core Studies

"In the preface to the first edition of The Physics of Glaciers, published in 1969, Stan Paterson made note of the impressive observational and theoretical advances that had taken place during the preceding two decades and set the stage for his efforts to summarize the state of the field. The pace of data collection has continued to accelerate with the development of an impressive array of new tools and techniques and the added incentive of current concerns over the response and role of glaciers and ice sheets in a warming climate. Now we arrive at the fourth edition, a collaborative effort by Paterson and Kurt Cuffey to provide an updated assessment of glacier physics and related topics. The result is a major achievement, involving a comprehensive rewriting and reorganization of the material contained in earlier editions, and including a significant amount of new material that will be appreciated by both old and new audiences."--Pure and Applied Geophysics "The interested reader will find much else to enjoy in this book. For example, by using square brackets for grouping, and curved parentheses for arguments of functions, the equations are easier to read than typical. The appendix on stress and strain will be a favorite of students in classes extending far beyond glaciology. In short, The Physics of Glaciers by Cuffey and Paterson is at once instructive and authoritative, a textbook and a reference source. It is a towering intellectual achievement that, quite simply, defines the science of glaciers. Modern students may not be as easily impressed as I was three decades ago, but I expect that in addition to bragging about talking to 'the W.S.B. Paterson', students will be celebrating meeting 'the K.M. Cuffey' for a long time to come."--Journal of Glaciology, Vol. 57, No. 202, 2011, page 383