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Mid-Latitude Weather Systems ReviewCarlson has written a profound book on synoptic systems. Unlike many meteorology texts, this book stresses physical understanding of synoptic systems through practical and lucid mathematical treatment. The physical insight Carlson provides so eloquently makes this an essential read for every student taking synoptic lab. Carlson explains abstruse topics (thermal vorticity for example) in a lucid and cogent manner. There are numerous case studies which are covered in depth and flow perfectly with the points Carlson wants to convey. The book does assume the reader has atleast a fundamental understanding of dynamics and thermo.I would consider this book to be a perfect supplement to Bluestein's Vol I, Chapter 5, which is a rigorous mathematical treatment of QG theory. It would also serve well as an alternative view of synoptic systems to Bluestein's Vol II since the way they approach topics are considerably different. This book is essential reading for the student and the professional in the field. I would consider this to be the best book I have ever read on the subject despite a few obvious errors. Below are a listing of the chapters in the book:
1. Introduction and mathematical definitions
2. Vorticity and vertical motion
3. The vorticity and thermodynamic equation
4. QG forcing of vertical motions and surface pressure tendency
5. QG energetics
6. Evolution and motion of mid-tropospheric waves: Barotropic viewpoint
7. Simple dynamic models of wave/cyclone Development: Baroclinic Viewpoint
8. Alternative expressions for vertical motion and divergence
9. Some additional dynamic aspects of the baroclinic wave/cyclone. Effects of friction, terrain, and diabatic heating
10. The evolution of cyclones
11. Evolution of the wave/cyclone during cyclogenesis
12. Optimum wavelength and growth rate of baroclinic waves
13. Airflow through mid-latitude synoptic-scale disturbances
14. Aegeostrophic and the dynamics of fronts
15. Upper tropospheric fronts and jet streaks
16. Mid-tropospheric fronts, elevated mixed layers and the severe storm environment
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