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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Format: | Article in Journal/Newspaper |
Language: | unknown |
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ODU Digital Commons
2006
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Online Access: | https://digitalcommons.odu.edu/ccpo_pubs/127 https://digitalcommons.odu.edu/cgi/viewcontent.cgi?article=1136&context=ccpo_pubs |