Geometry-dependent Ekman layer approximations on curved domains: L^{\infty} convergence

TL;DR

This paper investigates how the geometry of curved boundaries affects Ekman boundary layer approximations, providing convergence results in the L^{} norm without small-amplitude restrictions, and deriving boundary-dependent limiting systems.

Contribution

It introduces a geometric-dependent approximation framework for Ekman layers on curved domains and proves L^{} convergence, extending boundary layer theory beyond planar surfaces.

Findings

Convergence of approximate solutions in L^{} norm without small-amplitude assumptions.

Boundary geometry influences near-boundary flow structures.

Derived boundary-dependent limiting-state system in the vanishing-viscosity limit.

Abstract

The Ekman boundary layer is a fundamental concept in fluid dynamics that describes fluid motion near boundaries affected by Earth's rotation. Most theoretical studies have simplified their analysis by assuming a planar boundary surface, resulting in limited exploration of structures with general smooth boundary conditions. Investigating the impact of boundary geometry in the Ekman boundary layer is essential, as initially suggested by J.L. Lions and further examined in Masmoudi's study [Comm. Pure Appl. Math. 53 (2000), 432-483] under small amplitude periodic boundary conditions. This paper clarifies how boundary geometry influences flow fields and characterizes its effects on near-boundary layer flow. We construct a class of multi-scale approximate solutions based on the boundary's geometric features and establish their convergence in the L^{\infty} framework. Our findings do not require a small-amplitude assumption, only an upper bound on the Gaussian curvature of the boundary surface. Notably, when the boundary is planar, our approach aligns with existing studies. Additionally, in the vanishing-viscosity limit, we derive a limiting-state system dependent on boundary geometric parameters. These contributions extend the theoretical understanding of boundary-layer interactions to general curved geometries and have possible applications in atmospheric, oceanic, and other geophysical flow contexts.