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Microstructure Observations During the Spring 2011 Stratiphyt-ii Cruise in the Northeast Atlantic : Volume 9, Issue 3 (11/06/2012)

By Jurado, E.

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Book Id: WPLBN0003984666
Format Type: PDF Article :
File Size: Pages 34
Reproduction Date: 2015

Title: Microstructure Observations During the Spring 2011 Stratiphyt-ii Cruise in the Northeast Atlantic : Volume 9, Issue 3 (11/06/2012)  
Author: Jurado, E.
Volume: Vol. 9, Issue 3
Language: English
Subject: Science, Ocean, Science
Collections: Periodicals: Journal and Magazine Collection (Contemporary), Copernicus GmbH
Historic
Publication Date:
2012
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Van Der Woerd, H. J., Dijkstra, H. A., & Jurado, E. (2012). Microstructure Observations During the Spring 2011 Stratiphyt-ii Cruise in the Northeast Atlantic : Volume 9, Issue 3 (11/06/2012). Retrieved from http://www.ebooklibrary.org/


Description
Description: Institute for Marine and Atmospheric Research Utrecht (IMAU), Dept. of Physics and Astronomy, Utrecht University, Utrecht, The Netherlands. Small-scale temperature and conductivity variations have been measured in the upper 100 m of the Northeast Atlantic during the STRATIPHYT-II cruise (Las Palmas–Reykjavik, 6 April–3 May 2011). The measurements were done at midday and comprised 2 to 15 vertical profiles at each station. The derived turbulent quantities show a transition between weakly-stratified and well-mixed waters, which was centered at about 48° N. The temperature eddy diffusivities, KT, range from 10−5 to 100 m2s−1 in the weakly-stratified stations, and range from 3 × 10−4 to 2 × 100 m2s−1 in the well-mixed stations. The turbulent kinetic energy dissipation rates, ε, range from 3 × 10−8 to 2 × 10−6m2s−3 south of the transition zone, and from 10−7 to 10−5m2s−3 north of it. The station-averaged KT values throughout the mixed layer increase exponentially with the wind speed. The station-averaged ε values throughout the mixed layer scale with the wind stress similarity variable, u*3/(−Κ z), with a scaling factor of about 1.8 in the wind-dominated stations. The values of KT and ε are about 10 times higher compared to the values measured at the same stations in July 2009. The results presented here constitute a unique data set giving large spatial coverage of upper ocean spring turbulence quantities.

Summary
Microstructure observations during the spring 2011 STRATIPHYT-II cruise in the Northeast Atlantic

Excerpt
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