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Course in Dynamic Meteorology

Om Course in Dynamic Meteorology

Dynamic Meteorology is a fundamental branch of atmospheric science, which enables quantification of atmospheric motion to make accurate predictions of weather patterns. The book is designed as a text for students pursuing courses in Atmospheric Science, Meteorology, Oceanography, and Environmental Science at undergraduate and postgraduate level. The text is systematically developed with chapters on Sun, Earth and various physical processes involved in atmosphere. It assumes the reader to have basic knowledge of Calculus and Thermodynamiics and uses several approximations, without giving rigorous mathematical proofs, making the book simple and lucid. Features * Covers the complex subject of atmospheric processes in simple lucid way * General circulation of the atmosphere is described as zonal and meridional averages * Each chapter is followed by questions for self review

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  • Språk:
  • Engelsk
  • ISBN:
  • 9789352300006
  • Bindende:
  • Hardback
  • Sider:
  • 382
  • Utgitt:
  • 11 november 2014
  • Dimensjoner:
  • 165x241x30 mm.
  • Vekt:
  • 730 g.
  Gratis frakt
Leveringstid: 2-4 uker
Forventet levering: 26 oktober 2024

Beskrivelse av Course in Dynamic Meteorology

Dynamic Meteorology is a fundamental branch of atmospheric science, which enables quantification of atmospheric motion to make accurate predictions of weather patterns. The book is designed as a text for students pursuing courses in Atmospheric Science, Meteorology, Oceanography, and Environmental Science at undergraduate and postgraduate level.
The text is systematically developed with chapters on Sun, Earth and various physical processes involved in atmosphere. It assumes the reader to have basic knowledge of Calculus and Thermodynamiics and uses several approximations, without giving rigorous mathematical proofs, making the book simple and lucid.
Features
* Covers the complex subject of atmospheric processes in simple lucid way
* General circulation of the atmosphere is described as zonal and meridional averages
* Each chapter is followed by questions for self review

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