{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,20]],"date-time":"2026-03-20T01:23:41Z","timestamp":1773969821112,"version":"3.50.1"},"reference-count":46,"publisher":"American Geophysical Union (AGU)","issue":"C10","license":[{"start":{"date-parts":[[2006,10,7]],"date-time":"2006-10-07T00:00:00Z","timestamp":1160179200000},"content-version":"vor","delay-in-days":6,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["J. Geophys. Res."],"published-print":{"date-parts":[[2006,10]]},"abstract":"<jats:p>Ekman transport is studied close to the Galician coast by means of forecasted winds provided by METEOGALICIA from November 2001 to October 2004. Three different coastal zones are identified: western coast from Mi\u00f1o River to Cape Finisterre, middle coast from Cape Finisterre to Cape Ortegal and northern coast, from Cape Ortegal to Cape Pe\u00f1as. In addition to existence of long\u2010term variations, the periodicity of the transport signal is characterized by an annual component (365 days), a seasonal fluctuation (50 to 80 days) and a timescale related to passing storms (15\u201320 days). Although the periodicity of the signal is similar at the three zones owing to external meteorological forcing, the Ekman transport is modulated by the presence of the coast, in such a way that seasonal patterns vary in intensity and direction along the coast. Thus the autumn\u2010winter pattern is characterized by high transport at the northern and middle coast, pointing landward perpendicular to the shoreline, and moderate values at the western coast, pointing landward and oblique to the shoreline. On the other hand, the spring\u2010summer pattern is characterized by high transport at the western coast, pointing seaward perpendicular to the shoreline. The same orientation is observed at the middle coast although with a lower magnitude. Finally, Ekman transport at the northern coast points landward and oblique to the shoreline. The different transport orientations are shown to be responsible for the upwelling probability variation along the coast.<\/jats:p>","DOI":"10.1029\/2005jc003331","type":"journal-article","created":{"date-parts":[[2006,10,6]],"date-time":"2006-10-06T20:54:02Z","timestamp":1160168042000},"source":"Crossref","is-referenced-by-count":59,"title":["Ekman transport along the Galician coast (northwest Spain) calculated from forecasted winds"],"prefix":"10.1029","volume":"111","author":[{"given":"Moncho","family":"Gomez\u2010Gesteira","sequence":"first","affiliation":[{"name":"Grupo de F\u00edsica de la Atmosfera y del Oceano, Facultad de Ciencias, Campus de Ourense Universidad de Vigo  Ourense Spain"}]},{"given":"Camilo","family":"Moreira","sequence":"additional","affiliation":[{"name":"Grupo de F\u00edsica de la Atmosfera y del Oceano, Facultad de Ciencias, Campus de Ourense Universidad de Vigo  Ourense Spain"}]},{"given":"Ines","family":"Alvarez","sequence":"additional","affiliation":[{"name":"Grupo de F\u00edsica de la Atmosfera y del Oceano, Facultad de Ciencias, Campus de Ourense Universidad de Vigo  Ourense Spain"}]},{"given":"Maite","family":"deCastro","sequence":"additional","affiliation":[{"name":"Grupo de F\u00edsica de la Atmosfera y del Oceano, Facultad de Ciencias, Campus de Ourense Universidad de Vigo  Ourense Spain"}]}],"member":"13","published-online":{"date-parts":[[2006,10,7]]},"reference":[{"key":"e_1_2_6_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0272-7714(02)00309-8"},{"key":"e_1_2_6_3_1","doi-asserted-by":"publisher","DOI":"10.1029\/2004JC002504"},{"key":"e_1_2_6_4_1","doi-asserted-by":"publisher","DOI":"10.1029\/93JC00458"},{"key":"e_1_2_6_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0079-6611(01)00073-8"},{"key":"e_1_2_6_6_1","unstructured":"Bakun A.(1973) Coastal Upwelling Indexes west coast of North America 1946\u201371 NOAA Tech. Rep. NMFS 671 103 pp."},{"key":"e_1_2_6_7_1","doi-asserted-by":"publisher","DOI":"10.1002\/wea.6080581204"},{"key":"e_1_2_6_8_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0025-3227(97)00080-7"},{"key":"e_1_2_6_9_1","doi-asserted-by":"publisher","DOI":"10.1357\/002224087788401115"},{"key":"e_1_2_6_10_1","doi-asserted-by":"publisher","DOI":"10.1029\/93JC02735"},{"key":"e_1_2_6_11_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0967-0645(03)00125-5"},{"key":"e_1_2_6_12_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0493(2000)128<1632:LSSOTJ>2.0.CO;2"},{"key":"e_1_2_6_13_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0469(2001)058<1511:AOTMAB>2.0.CO;2"},{"issue":"11","key":"e_1_2_6_14_1","first-page":"1","article-title":"On the influence of Earth's rotation on ocean currents","volume":"2","author":"Ekman W. K.","year":"1905","journal-title":"Ark. Mat. Astron. Fys."},{"key":"e_1_2_6_15_1","volume-title":"Data Analysis Methods in Physical Oceanography","author":"Emery W. J.","year":"2001"},{"key":"e_1_2_6_16_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0485(1995)025<1651:EOWSAW>2.0.CO;2"},{"key":"e_1_2_6_17_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0485(1999)029<0177:TOTBUS>2.0.CO;2"},{"key":"e_1_2_6_18_1","unstructured":"Fiuza A. F. G.(1984) Hidrologia e dinamica das aguas costeiras de Portugal (Hydrology and dynamics of the Portuguese coastal water) Ph. D. dissertation 294 pp. Univ. de Lisboa Lisbon."},{"key":"e_1_2_6_19_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0967-0637(98)00008-9"},{"key":"e_1_2_6_20_1","doi-asserted-by":"publisher","DOI":"10.1029\/CO001p0176"},{"key":"e_1_2_6_21_1","doi-asserted-by":"publisher","DOI":"10.1029\/93JC02016"},{"key":"e_1_2_6_22_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF02803360"},{"key":"e_1_2_6_23_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0924-7963(02)00034-9"},{"key":"e_1_2_6_24_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0967-0637(03)00114-6"},{"key":"e_1_2_6_25_1","unstructured":"Lavin A. G.D\u00edaz del Rio J. M.Cabanas andG.Casas(1991) Afloramiento en el noroeste de la Peninsula Iberica: Indices de afloramiento para el punto 43\u00b0N 11\u00b0W periodo 1966\u20131989 Inf. Tec. Inst. Esp. Oceanogr.91 33 pp."},{"key":"e_1_2_6_26_1","first-page":"1","article-title":"Afloramiento en el noroeste de la Peninsula Iberica. Indices de afloramiento para el punto 43\u00b0N 11\u00b0W periodo 1990\u20131999","volume":"15","author":"Lavin A.","year":"2000","journal-title":"Datos Resumenes Inst. Esp. Oceanogr."},{"key":"e_1_2_6_27_1","first-page":"248","article-title":"Limitations of an objective weather\u2010typing system for the Iberian Peninsula","volume":"56","author":"Mart\u00edn\u2010Vide J.","year":"2001","journal-title":"Weather"},{"key":"e_1_2_6_28_1","doi-asserted-by":"publisher","DOI":"10.1006\/ecss.1999.0468"},{"key":"e_1_2_6_29_1","doi-asserted-by":"publisher","DOI":"10.1029\/2001JC001135"},{"key":"e_1_2_6_30_1","doi-asserted-by":"publisher","DOI":"10.1006\/ecss.1999.0550"},{"key":"e_1_2_6_31_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0967-0637(01)00023-1"},{"key":"e_1_2_6_32_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.jmarsys.2004.07.003"},{"key":"e_1_2_6_33_1","doi-asserted-by":"publisher","DOI":"10.1016\/0967-0637(95)00091-7"},{"key":"e_1_2_6_34_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0493(2004)132<2110:SAMWAW>2.0.CO;2"},{"key":"e_1_2_6_35_1","volume-title":"Introductory Dynamical Oceanography","author":"Pond S.","year":"1993"},{"key":"e_1_2_6_36_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0278-4343(96)00030-1"},{"key":"e_1_2_6_37_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0399-1784(98)80004-2"},{"key":"e_1_2_6_38_1","doi-asserted-by":"publisher","DOI":"10.1029\/2000JC000775"},{"key":"e_1_2_6_39_1","volume-title":"Numerical Recipes in C, The Art of Scientific Computing","author":"Press W. H.","year":"1992"},{"key":"e_1_2_6_40_1","doi-asserted-by":"publisher","DOI":"10.1093\/plankt\/21.1.21"},{"key":"e_1_2_6_41_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0924-7963(02)00250-6"},{"key":"e_1_2_6_42_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0450(2003)042<0129:IOCAON>2.0.CO;2"},{"key":"e_1_2_6_43_1","doi-asserted-by":"publisher","DOI":"10.1002\/j.1477-8696.2000.tb04023.x"},{"key":"e_1_2_6_44_1","first-page":"701","article-title":"Coastal upwelling in the Rias Bajas, NW Spain: Contrasting the benthic regimes of the Rias de Arosa and de Muros","volume":"40","author":"Tenore K. R.","year":"1982","journal-title":"J. Mar. Res."},{"key":"e_1_2_6_45_1","doi-asserted-by":"publisher","DOI":"10.1029\/2002JC001361"},{"key":"e_1_2_6_46_1","first-page":"131","article-title":"The seasonal upwelling cycle along the eastern boundary of the north Atlantic","volume":"34","author":"Wooster W. S.","year":"1976","journal-title":"J. Mar. Res."},{"key":"e_1_2_6_47_1","doi-asserted-by":"publisher","DOI":"10.1017\/S0022112003006244"}],"container-title":["Journal of Geophysical Research: Oceans"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/api.wiley.com\/onlinelibrary\/tdm\/v1\/articles\/10.1029%2F2005JC003331","content-type":"unspecified","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2005JC003331","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2023,10,12]],"date-time":"2023-10-12T21:40:22Z","timestamp":1697146822000},"score":1,"resource":{"primary":{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/2005JC003331"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2006,10]]},"references-count":46,"journal-issue":{"issue":"C10","published-print":{"date-parts":[[2006,10]]}},"alternative-id":["10.1029\/2005JC003331"],"URL":"https:\/\/doi.org\/10.1029\/2005jc003331","archive":["Portico"],"relation":{},"ISSN":["0148-0227"],"issn-type":[{"value":"0148-0227","type":"print"}],"subject":[],"published":{"date-parts":[[2006,10]]},"article-number":"2005JC003331"}}