Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer

We present an analysis of turbulent kinetic energy dissipation rates in the upper ocean using in situ measurements collected by a coherent Doppler sonar in the Labrador Sea during summer 2004. The sonar recorded horizontal velocity fluctuations of the upper 2 m with an uncommonly small spatial resol...

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Published in:The International Journal of Ocean and Climate Systems
Main Author: Gremes-Cordero, Silvia
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2017
Subjects:
Online Access:http://dx.doi.org/10.1177/1759313117744873
http://journals.sagepub.com/doi/pdf/10.1177/1759313117744873
http://journals.sagepub.com/doi/full-xml/10.1177/1759313117744873
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spelling crsagepubl:10.1177/1759313117744873 2023-05-15T17:06:07+02:00 Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer Gremes-Cordero, Silvia 2017 http://dx.doi.org/10.1177/1759313117744873 http://journals.sagepub.com/doi/pdf/10.1177/1759313117744873 http://journals.sagepub.com/doi/full-xml/10.1177/1759313117744873 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The International Journal of Ocean and Climate Systems volume 8, issue 3, page 161-172 ISSN 1759-3131 1759-314X General Medicine journal-article 2017 crsagepubl https://doi.org/10.1177/1759313117744873 2022-08-12T11:30:48Z We present an analysis of turbulent kinetic energy dissipation rates in the upper ocean using in situ measurements collected by a coherent Doppler sonar in the Labrador Sea during summer 2004. The sonar recorded horizontal velocity fluctuations of the upper 2 m with an uncommonly small spatial resolution of 0.8 cm, allowing direct calculations of wavenumber spectra and the application of Kolmogorov theory to obtain turbulent kinetic energy dissipation rates for the first time in this area. The project presented a unique opportunity for the study of air–sea exchange during a phytoplankton bloom, being the first time a specialized air–sea interaction spar buoy was deployed during such particular event. An additional uniqueness of this experiment resulted from being the first turbulent kinetic energy dissipation rate observations obtained at higher latitudes, coincidentally in a well-known region of dense water formation, with a fundamental role in both global circulation and forecasting studies of global climate change. Focusing on the relationship between turbulent kinetic energy dissipation rates and wave phase in the upper 2 m, we estimated O[Formula: see text] turbulent kinetic energy dissipation rates, consistent with previous estimates obtained through similar devices and methods. A T-test between dissipation rates calculated at the crest and at the trough of waves showed no dependency of turbulent kinetic energy dissipation rates on the wave phase at 2 m depth, coinciding with many of the earlier findings available. a comparison with previous research showing conflicting results with our values is also discussed here linking them to the relative roles of experimental design variations, diverse dynamical frames, and particular environmental conditions. Article in Journal/Newspaper Labrador Sea SAGE Publications (via Crossref) The International Journal of Ocean and Climate Systems 8 3 161 172
institution Open Polar
collection SAGE Publications (via Crossref)
op_collection_id crsagepubl
language English
topic General Medicine
spellingShingle General Medicine
Gremes-Cordero, Silvia
Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer
topic_facet General Medicine
description We present an analysis of turbulent kinetic energy dissipation rates in the upper ocean using in situ measurements collected by a coherent Doppler sonar in the Labrador Sea during summer 2004. The sonar recorded horizontal velocity fluctuations of the upper 2 m with an uncommonly small spatial resolution of 0.8 cm, allowing direct calculations of wavenumber spectra and the application of Kolmogorov theory to obtain turbulent kinetic energy dissipation rates for the first time in this area. The project presented a unique opportunity for the study of air–sea exchange during a phytoplankton bloom, being the first time a specialized air–sea interaction spar buoy was deployed during such particular event. An additional uniqueness of this experiment resulted from being the first turbulent kinetic energy dissipation rate observations obtained at higher latitudes, coincidentally in a well-known region of dense water formation, with a fundamental role in both global circulation and forecasting studies of global climate change. Focusing on the relationship between turbulent kinetic energy dissipation rates and wave phase in the upper 2 m, we estimated O[Formula: see text] turbulent kinetic energy dissipation rates, consistent with previous estimates obtained through similar devices and methods. A T-test between dissipation rates calculated at the crest and at the trough of waves showed no dependency of turbulent kinetic energy dissipation rates on the wave phase at 2 m depth, coinciding with many of the earlier findings available. a comparison with previous research showing conflicting results with our values is also discussed here linking them to the relative roles of experimental design variations, diverse dynamical frames, and particular environmental conditions.
format Article in Journal/Newspaper
author Gremes-Cordero, Silvia
author_facet Gremes-Cordero, Silvia
author_sort Gremes-Cordero, Silvia
title Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer
title_short Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer
title_full Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer
title_fullStr Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer
title_full_unstemmed Observations of turbulent kinetic energy dissipation at the Labrador Sea surface layer
title_sort observations of turbulent kinetic energy dissipation at the labrador sea surface layer
publisher SAGE Publications
publishDate 2017
url http://dx.doi.org/10.1177/1759313117744873
http://journals.sagepub.com/doi/pdf/10.1177/1759313117744873
http://journals.sagepub.com/doi/full-xml/10.1177/1759313117744873
genre Labrador Sea
genre_facet Labrador Sea
op_source The International Journal of Ocean and Climate Systems
volume 8, issue 3, page 161-172
ISSN 1759-3131 1759-314X
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/1759313117744873
container_title The International Journal of Ocean and Climate Systems
container_volume 8
container_issue 3
container_start_page 161
op_container_end_page 172
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