Reflection of nonlinear mountain waves by critical levels: behaviour of the reflection coefficient
Author:
Affiliation:
1. Department of MeteorologyUniversity of Reading Reading UK
2. Department of PhysicsUniversity of Algarve Faro Portugal
3. School of Atmospheric SciencesNanjing University Nanjing China
Publisher
Wiley
Subject
Atmospheric Science
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3722
Reference43 articles.
1. Argaín J.L.(2003).Numerical modelling of atmospheric flow: orographic and boundary layer effects. PhD thesis University of Algarve Faro Portugal.
2. Estimation of the Friction Velocity in Stably Stratified Boundary-Layer Flows Over Hills
3. Estimation of Surface-Layer Scaling Parameters in the Unstable Boundary Layer: Implications for Orographic Flow Speed-Up
4. On High-Drag States of Nonlinear Stratified Flow over an Obstacle
5. The critical layer for internal gravity waves in a shear flow
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2. Spectral steady-state solutions to the 2D compressible Euler equations for cross-mountain flows;Communications in Applied Mathematics and Computational Science;2021-06-22
3. The dependence of mountain wave reflection on the abruptness of atmospheric profile variations;Quarterly Journal of the Royal Meteorological Society;2020-02-28
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