Trapped mountain waves with a critical level just below the surface
Author:
Affiliation:
1. Laboratoire de Météorologie Dynamique, PSL Research University, Ecole Normale Suprieure, Paris
Publisher
Wiley
Subject
Atmospheric Science
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3507
Reference44 articles.
1. Form and wave drag due to stably stratified turbulent flow over low ridges
2. A new parametrization of turbulent orographic form drag
3. The critical layer for internal gravity waves in a shear flow
4. Parameterization of Orography-Induced Turbulence in a Mesobeta--Scale Model
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1. Mountain Waves Produced by a Stratified Shear Flow with a Boundary Layer. Part III: Trapped Lee Waves and Horizontal Momentum Transport;Journal of the Atmospheric Sciences;2022-06
2. The daytime trapped lee wave pattern and evolution induced by two small‐scale mountains of different heights;Quarterly Journal of the Royal Meteorological Society;2022-04
3. Impact of the Nocturnal Low-Level Jet and Orographic Waves on Turbulent Motions and Energy Fluxes in the Lower Atmospheric Boundary Layer;Boundary-Layer Meteorology;2021-06-08
4. A Large-Eddy Simulation Study on the Diurnally Evolving Nonlinear Trapped Lee Waves over a Two-Dimensional Steep Mountain;Journal of the Atmospheric Sciences;2021-02
5. Mountain Waves Produced by a Stratified Boundary Layer Flow. Part I: Hydrostatic Case;Journal of the Atmospheric Sciences;2020-05
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