Articles | Volume 15, issue 6
https://doi.org/10.5194/os-15-1439-2019
https://doi.org/10.5194/os-15-1439-2019
Research article
 | 
07 Nov 2019
Research article |  | 07 Nov 2019

Internal tide energy flux over a ridge measured by a co-located ocean glider and moored acoustic Doppler current profiler

Rob A. Hall, Barbara Berx, and Gillian M. Damerell

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Anna Wenzel on behalf of the Authors (23 May 2019)  Author's response
ED: Publish as is (03 Jun 2019) by Mattias Green
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Short summary
Internal tides are subsurface waves generated by tidal flows over ocean ridges. When they break they create turbulence that drives an upward flux of nutrients from the deep ocean to the nutrient-poor photic zone. Measuring internal tides is problematic because oceanographic moorings are often fished-out by commercial trawlers. We show that autonomous ocean gliders and acoustic Doppler current profilers can be used together to accurately measure the amount of energy carried by internal tides.