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Autor:
Gilcoto, M. (Miguel), Villacieros-Robineau, N. (Nicolás), Piñeiro, S. (Safo), Piedracoba, S. (Silvia), Rosón, G. (Gabriel), Torres, R. (Ricardo), Alonso-Pérez, F. (Fernando), Graña, R. (Rocío), Largier, J.L. (John), Barton, E.D. (Eric Desmond)
Publikováno v:
e-IEO. Repositorio Institucional Digital de Acceso Abierto del Instituto Español de Oceanografía
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The Ría de Vigo is a semi-enclosed bay in which tidal residual currents are associated with coastal upwelling events. Both upwelling and downwelling favourable winds generate a bidirectional exchange flow with the shelf – a two-layer circulation w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::6e56d74f12d023f8b88015fe3d371552
http://hdl.handle.net/10508/11839
http://hdl.handle.net/10508/11839
