Topographic Influence on Overflow Dynamics: Idealized Numerical Simulations and the Faroe Bank Channel Overflow

Properties of the North Atlantic Deep Water (NADW) depend on mixing that occurs in the Denmark Strait (DS) and the Faroe Bank Channel (FBC) overflow regions. How the sill's topography in those regions may affect mixing processes and downstream variability is thus investigated using a high-resol...

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Bibliographic Details
Main Author: Ezer, Tal
Format: Article in Journal/Newspaper
Language:unknown
Published: ODU Digital Commons 2006
Subjects:
Online Access:https://digitalcommons.odu.edu/ccpo_pubs/127
https://digitalcommons.odu.edu/cgi/viewcontent.cgi?article=1136&context=ccpo_pubs