OCES Departmental Seminar: Global overturning circulation constrained by tidal mixing map

4:00pm - 5:00pm
Zoom

Internal tides power much of the observed small-scale turbulence in the ocean interior. Here we present a global 3D map of tidal mixing that incorporates both the local and remote dissipation of internal tides. The map compares well with available mixing estimates across the globe. In light of this agreement, we combine the mixing map with the climatological density distribution of the ocean to estimate rates of upwelling across isopycnals. We find that tidal mixing (i) tends to homogenize North Atlantic Deep Water, (ii) sustains about 6 Sverdrups of upwelling near 4 km depth in the Indo-Pacific, and (iii) causes weak and uniform upwelling at mid-depths (1-2.5 km). The addition of geothermal heating boosts upwelling rates in the abyssal Pacific. However, upwelling at mid-depth remains unchanged and incompatible with popular figure-of-eight depictions of the global overturning circulation. An alternative schematic of the overturning is proposed.

Event Format
Speakers / Performers:
Casimir de Lavergne
LOCAEN, UPMC, Sorbonne University

Casimir de Lavergne is a CNRS researcher working at the LOCEAN laboratory hosted by Sorbonne University in Paris. His research focuses on the role of the deep and polar oceans in climate. Among his contributions feature studies of dense water formation in the Southern Ocean, Antarctic sea-ice trends and overturning circulation in the abyssal ocean. His most recent works explore the impacts of oceanic turbulence energized by tides, combining theory, observations and numerical models of the global ocean.

Language
English
More Information

(please contact jclmak@ust.hk for Zoom link)

Organizer
Department of Ocean Science
Contact

please contact jclmak@ust.hk for Zoom link

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