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Internal tides near a midlatitude shelf-slope front are studied using an idealized numerical model, with emphasis on their structure, energetics, and mixing effects. It is found that the properties of internal tides are highly dependent on frontal configuration and tidal frequency. At a winter front, energetic internal tides are generated and arrested in the frontal zone; the cross-shelf flow tends to be surface (bottom) intensified by a large internal circulation cell at the diurnaldoi:10.1175/1520-0485(2003)033<0170:amsoit>2.0.co;2 fatcat:uve4k42amnhklezaxoihscbknm