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

Autor(en)

Johannes Sachsperger, Stefano Serafin, Vanda Grubišić

Abstrakt

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.

Organisation(en)

Institut für Meteorologie und Geophysik

Journal

Frontiers in Earth Science

Band

3

Anzahl der Seiten

11

DOI

https://doi.org/10.3389/feart.2015.00070

Publikationsdatum

11-2015

Peer-reviewed

Ja

ÖFOS 2012

105206 Meteorologie

Schlagwörter

Link zum Portal

https://ucrisportal.univie.ac.at/de/publications/lee-waves-on-the-boundarylayer-inversion-and-their-dependence-on-freeatmospheric-stability(9f81aca4-0ca3-49bc-85dc-2391b1968e9f).html