@article{
 title = {Uso de un modelo de aguas someras para analizar la influencia del Atlántico Tropical Norte y del Pacıfico Ecuatorial del Este sobre la
      circulación atmosférica en los mares Intra-Americanos},
 type = {article},
 year = {2007},
 identifiers = {[object Object]},
 keywords = {crn2050},
 pages = {15-26},
 volume = {7},
 websites = {http://www.erevistas.csic.es/ficha_articulo.php?url=oai:home3.worldonline.es/jaguijar/reclim.html:10521&#38,oai_iden=oai_revista97,citeulike-article-id:6782618},
 id = {89aeeeaf-f628-3770-8959-a9bb87025f55},
 created = {2019-04-01T18:02:15.479Z},
 file_attached = {false},
 profile_id = {1f5347e3-dec5-3349-a941-3b484c2dfce9},
 group_id = {184ee5d4-bd93-3566-938b-14cc43849390},
 last_modified = {2019-04-01T18:02:15.479Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {false},
 hidden = {false},
 source_type = {JOUR},
 private_publication = {false},
 abstract = {A shallow water model was used to simulate the anomalous circulation over the Intra American Seas (IAS), due to
      heat forcing functions located at the Tropical North Atlantic and the Eastern Equatorial Pacific Oceans, respectively.
      Despite of its simplicity, the shallow water model represented the main features of the anomalous circulation
      over the IAS due to the heat forcing functions described previously. The main anomaly patterns were observed
      when heat sources have opposite signs across the IAS, e.g. Tropical North Atlantic cool (warm) and Eastern equatorial Pacific warn (cool). Results imply an increase (a decrease) in the vertical wind shear over the IAS for a cool (warm) Tropical North Atlantic and a warm (cool) Eastern Equatorial Pacific. These patterns could be associated with a larger (smaller) vertical wind shear over the IAS.},
 bibtype = {article},
 author = {Alfaro, E J and Hernández, D and Bezanilla, A},
 journal = {Revista de Climatologia}
}

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The main anomaly patterns were observed\n when heat sources have opposite signs across the IAS, e.g. Tropical North Atlantic cool (warm) and Eastern equatorial Pacific warn (cool). Results imply an increase (a decrease) in the vertical wind shear over the IAS for a cool (warm) Tropical North Atlantic and a warm (cool) Eastern Equatorial Pacific. 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The main anomaly patterns were observed\n when heat sources have opposite signs across the IAS, e.g. Tropical North Atlantic cool (warm) and Eastern equatorial Pacific warn (cool). Results imply an increase (a decrease) in the vertical wind shear over the IAS for a cool (warm) Tropical North Atlantic and a warm (cool) Eastern Equatorial Pacific. These patterns could be associated with a larger (smaller) vertical wind shear over the IAS.},\n bibtype = {article},\n author = {Alfaro, E J and Hernández, D and Bezanilla, A},\n journal = {Revista de Climatologia}\n}","author_short":["Alfaro, E., J.","Hernández, D.","Bezanilla, A."],"urls":{"Website":"http://www.erevistas.csic.es/ficha_articulo.php?url=oai:home3.worldonline.es/jaguijar/reclim.html:10521&#38,oai_iden=oai_revista97,citeulike-article-id:6782618"},"bibbaseid":"alfaro-hernndez-bezanilla-usodeunmodelodeaguassomerasparaanalizarlainfluenciadelatlnticotropicalnorteydelpacficoecuatorialdelestesobrelacirculacinatmosfricaenlosmaresintraamericanos-2007","role":"author","keyword":["crn2050"],"downloads":0},"search_terms":["uso","modelo","aguas","someras","para","analizar","influencia","del","atl","ntico","tropical","norte","del","pac","fico","ecuatorial","del","este","sobre","circulaci","atmosf","rica","los","mares","intra","americanos","alfaro","hernández","bezanilla"],"keywords":["crn2050"],"authorIDs":[]}