The air flow over a ridge — the effects of the upper boundary and high-level conditions-Reference-Cited by-同舟云学术

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The air flow over a ridge — the effects of the upper boundary and high-level conditions

Published:1958-01 Issue:359 Volume:84 Page:25-37
ISSN:0035-9009
Container-title:Quarterly Journal of the Royal Meteorological Society
language:en
Short-container-title:Q.J Royal Met. Soc.

Author:

Corby G. A.,Sawyer J. S.

Publisher

Wiley

Subject

Atmospheric Science

Reference8 articles.

1. Airflow over mountains: The lee-wave amplitude

2. 1932 Hydrodynamics, 6th Edn., Arts. 242–246.

3. 1947 ‘Theory of perturbations in stratified currents with applications to airflow over mountain barriers,’ Univ. Chicago Misc. Rep. Met. Dept., No. 23.

4. THE PHYSICAL AND DYNAMICAL PROBLEMS OF OROGRAPHIC RAIN

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1. Unusual Trapped Mountain Lee Waves with Deep Vertical Penetration and Significant Stratospheric Amplitude;Journal of the Atmospheric Sciences;2020-01-30

2. Does the stability above the upper boundary have any effect on the orographic rainfall?;Modeling Earth Systems and Environment;2016-04-07

3. The Dissipation of Trapped Lee Waves. Part I: Leakage of Inviscid Waves into the Stratosphere;Journal of the Atmospheric Sciences;2015-03-31

4. The Influence of Mountains on Airflow, Clouds, and Precipitation;Storm and Cloud Dynamics - The Dynamics of Clouds and Precipitating Mesoscale Systems;2011

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