Sea surface temperature anomalies in the Gulf of California

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Auteur principal: M. F. Lavín
Format: Artículo científico
Langue:en
Publié: Universidad Nacional Autónoma de México 2003
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_version_ 1876430206060724224
author M. F. Lavín
author_facet M. F. Lavín
contents Sea surface temperature anomalies in the Gulf of California M. F. Lavín C. Cabrera E. Palacios Hernández Ciencias de la Tierra El Niño interdecadal SST anomalies Gulf of California Satellite infrared images from January 1984 to December 2000 are used to describe interannual sea surface temperature(SST) anomalies in the Gulf of California. The predominant positive anomalies are due to El Niño, especially in 1997-1998, withdeviations of over 3°C from the seasonal climatology. The largest negative anomaly (~-4°C) was associated with La Niña of 1988-89. The 1986-87 El Niño had the weakest effect, with anomalies < 2 °C. The SST anomalies tend to be earlier and stronger in theregion just south of the mid-gulf archipelago; this may be due to the presence of strong SST fronts in that area. Some anomaliesappear to be connected to anomalies of the same sign in the Western Hemisphere Warm Pool of the eastern Pacific. Some anomalies,especially in the northern gulf, may be caused by local processes. The origin of some anomalies remain unknown. A statisticallysignificant warming of ~ 1°C during the 17 years of the record was observed, apparently within the interdecadal variabilityof the Pacific ocean. 2003 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56842308 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.3 Vol.42
format Artículo científico
id redalyc_56842308
institution Redalyc
language en
publishDate 2003
publisher Universidad Nacional Autónoma de México
spellingShingle Sea surface temperature anomalies in the Gulf of California
M. F. Lavín
Ciencias de la Tierra
El Niño
interdecadal
SST anomalies
Gulf of California
Sea surface temperature anomalies in the Gulf of California M. F. Lavín C. Cabrera E. Palacios Hernández Ciencias de la Tierra El Niño interdecadal SST anomalies Gulf of California Satellite infrared images from January 1984 to December 2000 are used to describe interannual sea surface temperature(SST) anomalies in the Gulf of California. The predominant positive anomalies are due to El Niño, especially in 1997-1998, withdeviations of over 3°C from the seasonal climatology. The largest negative anomaly (~-4°C) was associated with La Niña of 1988-89. The 1986-87 El Niño had the weakest effect, with anomalies < 2 °C. The SST anomalies tend to be earlier and stronger in theregion just south of the mid-gulf archipelago; this may be due to the presence of strong SST fronts in that area. Some anomaliesappear to be connected to anomalies of the same sign in the Western Hemisphere Warm Pool of the eastern Pacific. Some anomalies,especially in the northern gulf, may be caused by local processes. The origin of some anomalies remain unknown. A statisticallysignificant warming of ~ 1°C during the 17 years of the record was observed, apparently within the interdecadal variabilityof the Pacific ocean. 2003 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56842308 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.3 Vol.42
title Sea surface temperature anomalies in the Gulf of California
topic Ciencias de la Tierra
El Niño
interdecadal
SST anomalies
Gulf of California
url https://www.redalyc.org/articulo.oa?id=56842308