The Bottom Boundary Layer in the Eastern Tropical Pacific

Abstract

Vertical and horizontal structure of near-bottom currents at two locations in the eastern tropical Pacific (9°26?N, 151°17?W; 14°38?N, 125°29?W) have been studied. Low-frequency currents at these sites, located in a region of abyssal hills, increased between 500 m and 50 m above bottom and had small horizontal scale. Below 50 m frictional boundary-layer effects which were consistent with a simple, steady-state Ekman-like layer were apparent. Total veering within the boundary layer was, 10° counterclockwise (looking down) at both locations. High-frequency internal wave motions were consistent with a modified Garrelt and Munk internal wave spectrum. Energy correspondence calculations for several high-frequency bands showed some evidence for benthic internal wave generation by means of mean flow topography interaction. At the western site the near-inertial energy-time dependence and near-bottom enhancement both indicated local production in this band. Below 50 m frictional effects were again important. The observations showed veering and attenuation which depended on frequency and polarization in a manner consistent with time-dependent Ekman dynamics.