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Special Doppler lidar observations and numerical simulations with a grid spacing of 100 m were carried out focusing on the downslope winds around the Sendai airport on 14 February 2008. The model reproduced stationary lee waves with an approximate 20-km wavelength, consistent with the observed horizontal scale in water vapor images from the Japanese geostationary multifunctional transport satellite (MTSAT-1R). The simulated lee waves are accompanied by strong vertical shear, which leads to the separation of a vortex sheet from the surface, where small-scale vortices are generated successively. The vortex sheet is under favorable conditions for Kelvin-Helmholtz instability and may account for the generation of small-scale vortices. The simulated vortices, which are advected downstream, are accompanied by weak low-level wind patches. The Doppler lidar observation also captured the weak low-level wind patches with a horizontal scale of 1000-m moving downstream near the surface. An observed temporal variability in line-of-site wind speed decreased with increasing altitude from the surface. This feature was reproduced by the model in a qualitative sense, although the model tended to overestimate (underestimate) the variability below (above) a height of approximately 800 m."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658943098240","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"90466524"},{"@type":"NRID","@value":"1000090466524"},{"@type":"NRID","@value":"9000396132266"},{"@type":"NRID","@value":"9000257768062"},{"@type":"NRID","@value":"9000398304131"},{"@type":"NRID","@value":"9000324997414"}],"foaf:name":[{"@language":"en","@value":"SAWADA Masahiro"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Geophysics, Graduate School of Science, Tohoku 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