Formation of intrathermocline lenses by eddy–wind interaction
McGillicuddy, Dennis J.
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KeywordCirculation/ Dynamics; Eddies; Ekman pumping/transport; Mesoscale processes; Models and modeling; Ocean models; Primitive equations model
Mesoscale intrathermocline lenses are observed throughout the World Ocean and are commonly attributed to water mass anomalies advected from a distant origin. An alternative mechanism of local generation is offered herein, in which eddy–wind interaction can create lens-shaped disturbances in the thermocline. Numerical simulations illustrate how eddy–wind-driven upwelling in anticyclones can yield a convex lens reminiscent of a mode water eddy, whereas eddy–wind-driven downwelling in cyclones produces a concave lens that thins the mode water layer (a cyclonic “thinny”). Such transformations should be observable with long-term time series in the interiors of mesoscale eddies.
Author Posting. © American Meteorological Society, 2015. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 45 (2015): 606–612, doi:10.1175/JPO-D-14-0221.1.
Suggested CitationArticle: McGillicuddy, Dennis J., "Formation of intrathermocline lenses by eddy–wind interaction", Journal of Physical Oceanography 45 (2015): 606–612, DOI:10.1175/JPO-D-14-0221.1, https://hdl.handle.net/1912/7199
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