Citations: A Mountain Wave Theory including the Effect of the Vertical Variation of Wind and Stability1

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Z. Petkovšek & M. Ribaric. (1965) On the airflow over mountains with gentle slopes. Tellus 17:4, pages 443-448.
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Bo R. Döös. (1962) A theoretical analysis of lee wave clouds observed by Tiros I. Tellus 14:3, pages 301-309.
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Zeng-liang Zang, Ming Zhang & Hong Huang. (2007) Influence of the Scorer Parameter Profile on the Wavelength of Trapped Lee Waves. Journal of Hydrodynamics 19:2, pages 165-172.
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Takehiko Furukawa. (1973) Numerical Experiments of the Airflow over Mountains 1. Uniform current with constant static stability. Journal of the Meteorological Society of Japan. Ser. II 51:6, pages 400-419.
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Z. PETKOVŠEK & M. RIBARIČ. (1965) On the airflow over mountains with gentle slopes. Tellus 17:4, pages 443-448.
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Toshiyuki Kasai. (1965) Studies of Clouds Produced by Low Level Jets and Mountain Waves. Journal of the Meteorological Society of Japan. Ser. II 43:4, pages 196-205.
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T. N. Krishnamurti. (1964) Theory of two-dimensional mountain waves. Reviews of Geophysics 2:4, pages 593.
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BO R. DÖÖS. (1962) A theoretical analysis of lee wave clouds observed by Tiros I. Tellus 14:3, pages 301-309.
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A Mountain Wave Theory including the Effect of the Vertical Variation of Wind and StabilityFootnote¹
1 The research reported here has been sponsered in part by the Geophysics Research Directorate, AFCRL, AFRD, of the Air Research and Development Command, USAF, through its European office.

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A Mountain Wave Theory including the Effect of the Vertical Variation of Wind and StabilityFootnote11 The research reported here has been sponsered in part by the Geophysics Research Directorate, AFCRL, AFRD, of the Air Research and Development Command, USAF, through its European office.

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A Mountain Wave Theory including the Effect of the Vertical Variation of Wind and StabilityFootnote¹
1 The research reported here has been sponsered in part by the Geophysics Research Directorate, AFCRL, AFRD, of the Air Research and Development Command, USAF, through its European office.