Turbulent kinetic energy dissipation rate and associated fluxes in the western tropical Atlantic estimated from ocean glider observations

Sheehan, Peter M. F. ORCID: https://orcid.org/0000-0002-4906-5724, Damerell, Gillian M. ORCID: https://orcid.org/0000-0001-5808-0822, Leadbitter, Philip J., Heywood, Karen J. ORCID: https://orcid.org/0000-0001-9859-0026 and Hall, Rob A. ORCID: https://orcid.org/0000-0002-3665-6322 (2023) Turbulent kinetic energy dissipation rate and associated fluxes in the western tropical Atlantic estimated from ocean glider observations. Ocean Science, 19 (1). pp. 77-92. ISSN 1812-0784

[thumbnail of Turbulent kinetic energy dissipation rate and associated fluxes in the western tropical Atlantic estimated from ocean glider observations]
Preview
PDF (Turbulent kinetic energy dissipation rate and associated fluxes in the western tropical Atlantic estimated from ocean glider observations) - Published Version
Available under License Creative Commons Attribution.

Download (9MB) | Preview

Abstract

Ocean gliders enable us to collect the high-resolution microstructure observations necessary to calculate the dissipation rate of turbulent kinetic energy, ε, on timescales of weeks to months: far longer than is normally possible using traditional ship-based platforms. Slocum gliders have previously been used to this end; here, we report the first detailed estimates of ε calculated using the Batchelor spectrum method on observations collected by a FP07 fast thermistor mounted on a Seaglider. We use these same fast thermistor observations to calculate ε following the Thorpe scale method and find very good agreement between the two methods. The Thorpe scale method yields larger values of ε, but the average difference, which is less than an order of magnitude, is smaller than reported elsewhere. The spatio-temporal distribution of ε is comparable for both methods. Maximum values of ε (10−7 W kg−1) are observed in the surface mixed layer; values of approximately 10−9 W kg−1 are observed between approximately 200 and 500 m depth. These two layers are separated by a 100 m thick layer of low ε (10−10 W kg−1), which is co-located with a high-salinity layer of Subtropical Underwater and a peak in the strength of stratification. We calculate the turbulent heat and salt fluxes associated with the observed turbulence. Between 200 and 500 m, ε induces downward fluxes of both properties that, if typical of the annual average, would have a very small influence on the heat and salt content of the overlying salinity-maximum layer. We compare these turbulent fluxes with two estimates of double-diffusive fluxes that occur in regions susceptible to salt fingers, such as the western tropical Atlantic. We find that the double-diffusive fluxes of both heat and salt are larger than the corresponding turbulent fluxes.

Item Type: Article
Additional Information: Financial support: This research has been supported by the European Research Council (grant no. 741120) and UK Research and Innovation (grant no. NE/N012070/1).
Uncontrolled Keywords: oceanography,palaeontology ,/dk/atira/pure/subjectarea/asjc/1900/1910
Faculty \ School: Faculty of Science > School of Environmental Sciences
University of East Anglia Research Groups/Centres > Theme - ClimateUEA
UEA Research Groups: Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences
Faculty of Science > Research Groups > Collaborative Centre for Sustainable Use of the Seas
Related URLs:
Depositing User: LivePure Connector
Date Deposited: 25 Jan 2023 10:30
Last Modified: 05 Dec 2023 02:22
URI: https://ueaeprints.uea.ac.uk/id/eprint/90792
DOI: 10.5194/os-19-77-2023

Actions (login required)

View Item View Item