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Ocean eddies, fronts, and air-sea exchanges: Observations and high resolution simulations
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Eddy-induced cross-slope exchange in the northwestern Black Sea P-P4-04 Mengyao Ma* , 1st affiliation Feng zhou, Presenter Email: mmy@sio.org.cn |
Mesoscale eddies are frequently observed ocean processes at the shelf edge of the Black Sea. Remotely sensed high-resolution chlorophyll a and altimetry data have been used to investigate the development and migration of the mesoscale eddies in the northwestern Black Sea, along with a 3D circulation model output in this study. More than 15,000 eddies of different signs were identified in 2002–2010, with 53% of them appearing from March to July. During these periods, eddy-induced exchange accounts for 16%–31% of the total cross-slope volume transport at the upper layers shallower than 20 m. About volume of northwestern-shelf water was renewed by a single mesoscale eddy over the period 5 May to 20 July 2005, which is equivalent to 30.9% of the overall volume of shelf water |
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