Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 142: 1201–1212, April 2016 A DOI:10.1002/qj.2746 Dynamics of rotor formation in uniformly stratified two-dimensional flow over a mountain Johannes Sachsperger,a* Stefano Serafina and Vanda Grubisiˇ c´b,† aDepartment of Meteorology and Geophysics, University of Vienna, Austria bNational Center for Atmospheric Research‡, Boulder, CO, USA *Correspondence to: J. Sachsperger, Department of Meteorology and Geophysics, University of Vienna, Althanstraße 14 UZA2, 1090 Vienna, Austria. E-mail:
[email protected] †Additional affiliation: Department of Meteorology and Geophysics, University of Vienna, Austria ‡The National Center for Atmospheric Research is sponsored by the National Science Foundation The coupling between mountain waves in the free atmosphere and rotors in the boundary layer is investigated using a two-dimensional numerical model and linear wave theory. Uniformly stratified flow past a single mountain is examined. Depending on background stratification and mountain width, different wave regimes are simulated, from weakly to strongly nonlinear and from hydrostatic to non-hydrostatic. Acting in conjunction with surface friction, mountain waves cause the boundary layer to separate from the ground, causing the development of atmospheric rotors in the majority of the simulated flows. The rotors with largest vertical extent and strongest reverse flow near the ground are found to develop when the wave field is nonlinear and moderately non-hydrostatic, in line with linear theory predictions showing that the largest wave amplitudes develop in such conditions. In contrast, in near-hydrostatic flows boundary-layer rotors form even if the wave amplitude predicted by linear theory is relatively small.