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Secondary upwelling over a smooth shelf break
Institution:2. School of Mathematics and Physics, University of East Anglia, Norwich NR4 7TJ,U.K.;1. Institute of Marine Research, and Bjerknes Center for Climate Research, Bergen, Norway;2. NORCE Norwegian Research Centre, and Bjerknes Centre for Climate Research, Bergen, Norway;3. Nansen Environmental and Remote Sensing Center, and Bjerknes Centre for Climate Research, Bergen, Norway;4. Geophysical Institute, University of Bergen, and Bjerknes Centre for Climate Research, Bergen, Norway;5. Institute of Marine Research, Bergen, Norway;1. State Key Laboratory of Tropical Oceanography & Key Laboratory of Science and Technology on Operational Oceanography, South China Sea Institute of Oceanology & Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou, China;2. University of Chinese Academy of Sciences, Beijing, China;3. Southern Marine Science and Engineering Guangdong Laboratory, Guangzhou, China;4. Key Laboratory of Microwave Remote Sensing, National Space Science Center, Chinese Academy of Sciences, Beijing, China;5. National Satellite Ocean Application Service, Beijing, China;6. Shanghai Institute of Technical Physics, Chinese Academy of Sciences, Shanghai, China;7. Innovation Academy for Microsatellites, Chinese Academy of Sciences, Shanghai, China;1. Universidad Austral de Chile, Instituto de Acuicultura and Research center on Dynamics of High Latitude Marine Ecosystems (IDEAL), Avenida El Bosque 01789 Punta Arenas, Chile;2. Centro de Estudios de Algas Nocivas (CREAN), Instituto de Fomento Pesquero (IFOP), Enrique Abello 0552, Punta Arenas, Chile;3. Cape Horn International Center (CHIC), Universidad de Magallanes, Puerto Williams, Chile;4. Centro de Investigación GAIA Antártica (CIGA), Universidad de Magallanes, Av. Bulnes 01855, Punta Arenas, Chile;5. Millennium Institute Biodiversity of Antarctic and Subantarctic Ecosystem (BASE), Las Palmeras 3425, Santiago, Chile;1. State Key Laboratory of Marine Environmental Science, and Department of Physical Oceanography, College of Ocean and Earth Sciences, Xiamen University, Xiamen, Fujian 361102, China;2. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, Guangdong 519000, China;3. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA;4. Fujian Engineering Research Center for Ocean Remote Sensing Big Data, Xiamen, Fujian 361102, China;1. Department of Applied Physics, Faculty of Marine and Environmental Sciences, Marine Research Institute (INMAR), International Campus of Excellence of the Sea (CEI·MAR), University of Cadiz, Puerto Real, 11510 Cadiz, Spain;2. Department of Biology, Faculty of Marine and Environmental Sciences, Marine Research Institute (INMAR), International Campus of Excellence of the Sea (CEI·MAR), University of Cadiz, Puerto Real, 11510 Cadiz, Spain;3. Department of Mathematics and Statistics, University of Strathclyde, G1 1XH Glasgow, United Kingdom;4. Marine Hydrographic Institute (IHM), Spanish Navy, Division of Naval Support and Oceanography, Plaza San Severiano 3, 11007 Cadiz, Spain;5. Royal Netherlands Institute for Sea Research (NIOZ), P.O. Box 59, 1790 AB Den Burg, The Netherlands
Abstract:An unsteady model of secondary upwelling over the break at the edge of the continental shelf is described for bottom topography with a smooth but distinct shelf break. Numerical solutions are determined for examples using (i) a simple spin-up wind to illustrate the circulation and (ii) a moving pulse of wind to generate continental shelf waves.
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