The Coupled Ocean-Atmosphere Response to Small-Scale Atmospheric Jets
Abstract
The long-term goal of this project is to better understand the general problem of ocean-atmosphere interaction on small space and time scales. The present study has focused on gaining a better understanding the coupled response to small-scale atmospheric jets and oceanic surface fronts that are commonly observed near orographic features such as islands and mountain passes. The atmospheric response to sharp SST gradients has been explored in the strong wind regime, defined as U/fL>1, where U is the wind speed, f is the Coriolis parameter, and L is the ocean front width. Adjustments to the atmospheric boundary layer thickness, surface wind speed, and momentum balances are studied for both cold to warm and warm to cold winds. In a second study, it is shown that this feedback between ocean SST and surface winds can either enhance or reduce the growth rate and wavelengths of baroclinically unstable waves in the ocean, depending on wind direction. This coupling is most effective for low latitude, strongly stratified flows.
Document Details
- Document Type
- Technical Report
- Publication Date
- Mar 01, 2007
- Accession Number
- ADA465286
Entities
People
- Michael A. Spall
Organizations
- Woods Hole Oceanographic Institution