A generalized theory of flow forcing by rough topography

An analytical model is developed which explores the impact of irregular sea-floor roughness on large-scale oceanic flows. The previously reported asymptotic sandpaper' theory of flow-topography interaction represents relatively swift currents and exhibits singular behaviour in the weak flow limit. The present investigation systematically spans a wider parameter space and identifies the principal dissimilarities in the topographic regulation of slow and fast currents. The fast flows are controlled by the Reynolds stresses produced by topographically generated eddies. In contrast, relatively weak flows are more affected by the eddy-induced bottom form drag. The asymptotic models for fast and slow currents are then combined to arrive at a concise description of flow forcing by small-scale topography in homogeneous and multilayer models. The proposed closure is validated by comparing corresponding topography-resolving and parametric simulations.

Automated summary

An analytical model is developed to explore the impact of irregular sea-floor roughness on large-scale oceanic flows. The study systematically investigates the principal dissimilarities in the topographic regulation of slow and fast currents. It is found that fast flows are controlled by the Reynolds stresses produced by topographically generated eddies, while relatively weak flows are more affected by the eddy-induced bottom form drag. The combined asymptotic models for fast and slow currents provide a concise description of flow forcing by small-scale topography in homogeneous and multilayer models, which is validated through simulations.