Partly standing internal tides in a dendritic submarine canyon observed by an ocean glider
Partly standing internal tides in a dendritic submarine canyon observed by an ocean glider
An autonomous ocean glider is used to make the first direct measurements of internal tides within Whittard Canyon, a large, dendritic submarine canyon system that incises the Celtic Sea continental slope and a site of high benthic biodiversity. This is the first time a glider has been used for targeted observations of internal tides in a submarine canyon. Vertical isopycnal displacement observations at different stations fit a one-dimensional model of partly standing semidiurnal internal tides – comprised of a major, incident wave propagating up the canyon limbs and a minor wave reflected back down-canyon by steep, supercritical bathymetry near the canyon heads. The up-canyon internal tide energy flux in the primary study limb decreases from 9.2 to 2.0 kW m−1 over 28 km (a dissipation rate of
1−2.5×10−7Wkg−1
), comparable to elevated energy fluxes and internal tide driven mixing measured in other canyon systems. Within Whittard Canyon, enhanced mixing is inferred from collapsed temperature-salinity curves and weakened dissolved oxygen concentration gradients near the canyon heads. It has previously been hypothesised that internal tides impact benthic fauna through elevated near-bottom current velocities and particle resuspension. In support of this, we infer order 20 cm s−1 near-bottom current velocities in the canyon and observe high concentrations of suspended particulate matter. The glider observations are also used to estimate a 1 °C temperature range and 12 μmol kg−1 dissolved oxygen concentration range, experienced twice a day by organisms on the canyon walls, due to the presence of internal tides. This study highlights how a well-designed glider mission, incorporating a series of tide-resolving stations at key locations, can be used to understand internal tide dynamics in a region of complex topography, a sampling strategy that is applicable to continental shelves and slopes worldwide.
73-84
Hall, Rob A.
2a3a90bb-b421-4487-8f38-c114ac0b7ed7
Aslam, Tahmeena
5ef0448d-eac7-4985-9cfb-cfa18f229f9c
Huvenne, Veerle A.I.
f22be3e2-708c-491b-b985-a438470fa053
1 August 2017
Hall, Rob A.
2a3a90bb-b421-4487-8f38-c114ac0b7ed7
Aslam, Tahmeena
5ef0448d-eac7-4985-9cfb-cfa18f229f9c
Huvenne, Veerle A.I.
f22be3e2-708c-491b-b985-a438470fa053
Hall, Rob A., Aslam, Tahmeena and Huvenne, Veerle A.I.
(2017)
Partly standing internal tides in a dendritic submarine canyon observed by an ocean glider.
Deep Sea Research Part I: Oceanographic Research Papers, 126, .
(doi:10.1016/j.dsr.2017.05.015).
Abstract
An autonomous ocean glider is used to make the first direct measurements of internal tides within Whittard Canyon, a large, dendritic submarine canyon system that incises the Celtic Sea continental slope and a site of high benthic biodiversity. This is the first time a glider has been used for targeted observations of internal tides in a submarine canyon. Vertical isopycnal displacement observations at different stations fit a one-dimensional model of partly standing semidiurnal internal tides – comprised of a major, incident wave propagating up the canyon limbs and a minor wave reflected back down-canyon by steep, supercritical bathymetry near the canyon heads. The up-canyon internal tide energy flux in the primary study limb decreases from 9.2 to 2.0 kW m−1 over 28 km (a dissipation rate of
1−2.5×10−7Wkg−1
), comparable to elevated energy fluxes and internal tide driven mixing measured in other canyon systems. Within Whittard Canyon, enhanced mixing is inferred from collapsed temperature-salinity curves and weakened dissolved oxygen concentration gradients near the canyon heads. It has previously been hypothesised that internal tides impact benthic fauna through elevated near-bottom current velocities and particle resuspension. In support of this, we infer order 20 cm s−1 near-bottom current velocities in the canyon and observe high concentrations of suspended particulate matter. The glider observations are also used to estimate a 1 °C temperature range and 12 μmol kg−1 dissolved oxygen concentration range, experienced twice a day by organisms on the canyon walls, due to the presence of internal tides. This study highlights how a well-designed glider mission, incorporating a series of tide-resolving stations at key locations, can be used to understand internal tide dynamics in a region of complex topography, a sampling strategy that is applicable to continental shelves and slopes worldwide.
Text
Hall_et_al_2017_Partly_standing_internal_tides_DSRI_authors_copy
- Accepted Manuscript
More information
Accepted/In Press date: 31 May 2017
Published date: 1 August 2017
Identifiers
Local EPrints ID: 413168
URI: http://eprints.soton.ac.uk/id/eprint/413168
ISSN: 0967-0637
PURE UUID: ff08b01d-900e-45a3-9dd8-9b2227efe566
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Date deposited: 17 Aug 2017 16:30
Last modified: 16 Mar 2024 05:39
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Author:
Rob A. Hall
Author:
Tahmeena Aslam
Author:
Veerle A.I. Huvenne
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