The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments

Photosynthetic pigment concentrations retrieved from data generated from 1978 to 1986 by the sensor Coastal Zane Color Scanner were used to describe the seasonal and interannual variation of phytoplankton biomass of the Gulf of Tehuantepec and adjacent areas. The pigment concentrations 0.3 mg m–3 an...

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Autores principales: Lluch-Cota, SE, Álvarez-Borrego, S, Santamaría-Ángel, E, Müller-Karger, F, Hernández-Vázquez, S
Formato: Online
Lenguaje:eng
Publicado: Iniversidad Autónoma de Baja California 1997
Acceso en línea:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/809
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spelling oai:cienciasmarinas.com.mx:article-8092019-05-22T21:09:46Z The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments El golfo de Tehuantepec y áreas adyacentes: variación espaciotemporal de pigmentos fotosintéticos derivados de satélite Lluch-Cota, SE Álvarez-Borrego, S Santamaría-Ángel, E Müller-Karger, F Hernández-Vázquez, S Gulf of Tehuantepec photosynthetic pigments satellite data CZCS Golfo de Tehuantepec pigmentos fotosintéticos datos de satélite CZCS Photosynthetic pigment concentrations retrieved from data generated from 1978 to 1986 by the sensor Coastal Zane Color Scanner were used to describe the seasonal and interannual variation of phytoplankton biomass of the Gulf of Tehuantepec and adjacent areas. The pigment concentrations 0.3 mg m–3 and higher were considered as an index of productive waters. Its spatial coverage shows coastal upwelling in the gulfs of Tehuantepec and Papagayo (in the eastern region of the study area) between October and April. upwelling at the Costa Rica dome during summer. and the transient effect of mixing by tropical storms from July to October throughout the study area. Upwelling events in Tehuantepec and Central America are not synchronous. The region west of the Gulf of Tehuantepec is oligotrophic most of the time (less than 0.2 mg m–3). The most evident interannual variation was the effect of El Niño 1982–1983, with very low pigment concentrations associated with a deep thermocline in the whole study area. Also, there was an anti-El Niño event in 1985 in the eastern region, with high phytoplankton biomass concentrations associated with a shallow thermocline Mediante el uso de datos de concentración de pigmentos fotosintéticos generados por el sensor Coastal Zone Color Scanner de 1978 a 1986, se describe la variación estacional e interanual de la biomasa fitoplanctónica del Golfo de Tehuantepec y zonas adyacentes. Las concentraciones de 0.3 mg m–3 y mayores fueron consideradas como índice de aguas productivas. Su cobertura espacial muestra las surgencias costeras de los golfos de Tehuantepec y Papagayo (en la región oriental del área de estudio) entre octubre y abril, la surgencia del domo de Costa Rica en verano y el efecto episódico de mezcla por tormentas tropicales de julio a octubre en toda el área de estudio. Los eventos de surgencia de Tehuantepec y Centroamérica no son sincrónicos. La región al occidente de Tehuantepec es oligotrófíca la mayor parte del tiempo (menor que 0.2 mg mm–3). La variación interanual mas evidente fue el efecto de El Niño 1982–1983, con muy bajas concentraciones de pigmentos asociadas con una termoclina profunda en toda el área de estudio. Además, hubo un evento anti-El Niño en 1985 en la región oriental, con concentraciones elevadas de biomasa fìtoplanctónica asociadas con una termoclina somera. Iniversidad Autónoma de Baja California 1997-03-06 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article Artículo Arbitrado application/pdf https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/809 10.7773/cm.v23i3.809 Ciencias Marinas; Vol. 23 No. 3 (1997); 329-340 Ciencias Marinas; Vol. 23 Núm. 3 (1997); 329-340 2395-9053 0185-3880 eng https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/809/1068
institution Ciencias Marinas
collection OJS
language eng
format Online
author Lluch-Cota, SE
Álvarez-Borrego, S
Santamaría-Ángel, E
Müller-Karger, F
Hernández-Vázquez, S
spellingShingle Lluch-Cota, SE
Álvarez-Borrego, S
Santamaría-Ángel, E
Müller-Karger, F
Hernández-Vázquez, S
The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments
author_facet Lluch-Cota, SE
Álvarez-Borrego, S
Santamaría-Ángel, E
Müller-Karger, F
Hernández-Vázquez, S
author_sort Lluch-Cota, SE
title The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments
title_short The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments
title_full The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments
title_fullStr The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments
title_full_unstemmed The Gulf of Tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments
title_sort gulf of tehuantepec and adjacent areas: spatial and temporal variation of satellite-derived photosynthetic pigments
description Photosynthetic pigment concentrations retrieved from data generated from 1978 to 1986 by the sensor Coastal Zane Color Scanner were used to describe the seasonal and interannual variation of phytoplankton biomass of the Gulf of Tehuantepec and adjacent areas. The pigment concentrations 0.3 mg m–3 and higher were considered as an index of productive waters. Its spatial coverage shows coastal upwelling in the gulfs of Tehuantepec and Papagayo (in the eastern region of the study area) between October and April. upwelling at the Costa Rica dome during summer. and the transient effect of mixing by tropical storms from July to October throughout the study area. Upwelling events in Tehuantepec and Central America are not synchronous. The region west of the Gulf of Tehuantepec is oligotrophic most of the time (less than 0.2 mg m–3). The most evident interannual variation was the effect of El Niño 1982–1983, with very low pigment concentrations associated with a deep thermocline in the whole study area. Also, there was an anti-El Niño event in 1985 in the eastern region, with high phytoplankton biomass concentrations associated with a shallow thermocline
publisher Iniversidad Autónoma de Baja California
publishDate 1997
url https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/809
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