Dense Outflows and Deep Convection in the Antarctic Zone of the Southern Ocean
Abstract
This project seeks to quantify and better define the dynamics of those processes, including mixing, tides, current-topography interactions and nonlinear equation of state phenomena, that impact vertical transports of heat and mass in the Southern Ocean. These transports are crucial to the formation of Antarctic Bottom Water (AABW) and are integral to the Southern Ocean branch of the meridional overturning circulation (MOC). Improved understanding of the related processes will enhance our ability to predict climate-related changes in the MOC.
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 30, 2008
- Accession Number
- ADA534249
Entities
People
- Robin D. Muench