Show simple item record

contributor authorLueck, Rolf G.
contributor authorCrawford, William R.
contributor authorOsborn, Thomas R.
date accessioned2017-06-09T14:46:46Z
date available2017-06-09T14:46:46Z
date copyright1983/10/01
date issued1983
identifier issn0022-3670
identifier otherams-26587.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163497
description abstractThirteen profiles of the rate of viscous dissipation of turbulent kinetic energy &epsi? were made over the continental slope off Vancouver Island between 12 and 14 May 1980 in conjunction with CTD and moored current-meter observations. Systematic variability was observed in the vertical but not in the horizontal direction. Above 200 m depth numerous salt-stabilized temperature inversions were seen and dissipation rates were significantly larger than below 200 m. Dissipation rates below 200 m are the lowest ever reported and coincide with a low level of energetics revealed by the current meter moorings. Comparison with the Garrett-Munk internal wave spectrum indicates an e-folding decay time of internal wave energy of ?50 days at depths below 200 m.
publisherAmerican Meteorological Society
titleTurbulent Dissipation Over the Continental Slope Off Vancouver Island
typeJournal Paper
journal volume13
journal issue10
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1983)013<1809:TDOTCS>2.0.CO;2
journal fristpage1809
journal lastpage1818
treeJournal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 010
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record