Entrainment in the Denmark Strait overflow plume by meso-scale eddies

The entrainment of buoyant ambient water into the overflow plume of Denmark Strait and the associated downstream warming of the plume are estimated using time series of currents and temperature from moored instrumentation and classical hydrographic data. Warming rates are highest (0.4–0.5 K/100 km)...

Full description

Bibliographic Details
Main Authors: G. Voet, D. Quadfasel
Format: Article
Language:English
Published: Copernicus Publications 2010-03-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/6/301/2010/os-6-301-2010.pdf