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Customer Reviews:Average Customer Rating: predictor for one's success in atmospheric sciences I was trained in a classical program in atmospheric sciences in the sense that the atmosphere is a fluid hence the field being a sub-discipline of fluid mechanics is much emphasized. Holton's book is The Undergraduate Textbook for programs rooted in this understanding, in the US or internationally. Extraordinarily good text I have to say I'm not sure if texts on atmospheric dynamics get better than this. Physics books in general, in fact, rarely provide an understanding of phenomena that is so concise, intuitive, and yet mathematically robust. I highly recommend it for children, as a gift, and for pleasure reading. feedback from rmd it's a very analytic book; it's strongly related to anaysis. all the models are very well explaned; perhaps there is not a good relationship between models and pratical meteorology. phenomena are quite 'hidden' by equations, and only a good experienced physicist has the tools to extract the pratical approach deriving from model behaviours. The most exellent textbook in dynamics of the atmopshere This book, in my opinion, is the most valuable book on dynamical aspects of the atmosphere insofar, especially from pedagogical point of views. As a foreign student, I understand well Holton's writings. Simple but very concise sentences, no wordy explanations. The first 3 chapters provide you the basic equations used in meteorology and their common approximations. The next 5 chapters, to me, are the most interesting chapters. They give you wide range of knowledge from boundary layer, synoptic scale phenomena, to instabilities. Equations are of great usefulness because THEY bring into the light physical contents of the dynamics of the atmosphere. To me, any analytical equation and its explicit solution provide us a more complete understanding than numerical models do (because you never know some unpredictable behaviour of numerical solutions). So, try to understand carefully the simplest cases that Holton selected. This gives you a lot of deeper understandings. Chapters 9 to 11 provide the dynamics of meso- to large-scale circulations. You will see why the Hadley circulation descends around 35N in very clear way. However, simple Poisson eqn with the argument of "positive forcing, negative solution" that is applied throughout the text should be paid especial attention because this conclusion is not always true. As a whole, the contents, explanations and derivations will be very well constructed if you see the main point of each section. you can't find an alternative. when i was a student, i used to think, like many other reviewers, that the book is extremely dry. but now as a researcher in atmospheric-oceanic dynamics, i realise that the book is useful in explaining the most essential and elementary theories behind the dynamics one can encounter in meteorology or climate dynamics. | | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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