Lee Waves on the Boundary-Layer Inversion and Their Dependence on Free-Atmospheric Stability

Frontiers in Digital Humanities

Sachsperger, Johannes¹  Serafin, Stefano¹  GrubiÅ¡ić, Vanda¹ 

[1] Department of Meteorology and Geophysics, University of Vienna, Vienna, Austria

关键词: Trapped lee waves;    Water Waves;    boundary layer;    Inversion layer;    Stratified flow;   

DOI  :  10.3389/feart.2015.00070

学科分类：社会科学、人文和艺术（综合）

来源: Frontiers

【 摘 要 】

This study examines gravity waves that develop at the boundary-layer capping inversion in the lee of a mountain ridge. By comparing different linear wave theories, we show that lee waves that form under these conditions are most accurately described as forced interfacial waves. Perturbations in this type of flow can be studied with a linear two-dimensional model with constant wind speed and a sharp density discontinuity separating two layers, a neutral one below and a stable one above. Defining the model parameters on the basis of observations taken in the Madeira archipelago, we highlight the impact of upper-level stability on interfacial waves. We demonstrate that stable stratification aloft limits the possible range of lee wavelengths and modulates the length of the stationary wave mode. Finally, we show that the stable stratification aloft strongly constrains the validity of the shallow-water (or long-wave) approximation by permitting only short-wave modes to be trapped at the interface.

【 授权许可】

CC BY