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Stratified flow over a mountain with a gap: Linear theory and numerical simulations

Linear theory and numerical simulations are used to investigate gap flows. Both gaps embedded in a long mountain ridge and gaps located between two isolated mountain peaks are considered. The study mainly focuses on level gaps so as to isolate three‐dimensional effects from two‐dimensional gravity‐wave propagation. Special attention is given to qualitative differences between the linear and the nonlinear flow regimes, the linear regime being defined by the absence of gravity‐wave breaking.