2001
DOI: 10.7773/cm.v27i3.490
|View full text |Cite
|
Sign up to set email alerts
|

Temperature, Salinity, Nutrients And Chlorophyll a In Coastal Waters Of The Southern California Bight

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
7
0
1

Year Published

2008
2008
2023
2023

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 22 publications
(11 citation statements)
references
References 20 publications
0
7
0
1
Order By: Relevance
“…Sediment transport into and within the bay follows the same circulation pattern [25]. The bay is under the upwelling influence during periods of NW winds, a prominent feature of much of the Pacific coast of the USA and northern Baja California [26], and some authors have documented the influence of the local upwelling on water properties near the mouth during the springtime upwelling period [22] [27].…”
Section: Study Sitementioning
confidence: 95%
“…Sediment transport into and within the bay follows the same circulation pattern [25]. The bay is under the upwelling influence during periods of NW winds, a prominent feature of much of the Pacific coast of the USA and northern Baja California [26], and some authors have documented the influence of the local upwelling on water properties near the mouth during the springtime upwelling period [22] [27].…”
Section: Study Sitementioning
confidence: 95%
“…Outside of TSB, northwesterly winds also cause an offshore Ekman transport that results in year-round upwelling of cold, relatively saline and nutrientrich waters (Zaytsev et al, 2003); however, the magnitude and frequency of coastal upwelling are higher in the spring and summer (Gómez-Valdéz, 1983;Pérez-Brunius et al, 2007). Upwelling events and fluctuations in the flow of the California Current control the physical and chemical variability of the water column (i.e., salinity, temperature, and nutrients; Espinosa-Carreón et al, 2001;Pérez-Brunius et al, 2006;Linacre et al, 2010), primary production rates (Espinosa-Carreón et al, 2001, as well as the occurrence of algal blooms both outside and inside TSB, with a high likelihood of toxic blooms inside the bay (Peña-Manjarrez et al, 2005;García-Mendoza et al, 2009;Berdalet et al, 2014).…”
Section: Description Of the Study Sitementioning
confidence: 99%
“…Las concentraciones medias de nutrientes fueron de 3.31 µM para el DIN y de 0.83 µM para el DIP. Sin embargo, antes de los florecimientos y durante la primavera de cada año, a Different local sources of DIP and DIN exist in TSB: coastal upwelling waters transported to the inner bay (Espinosa-Carreón 2001, Segovia-Zavala et al 2007, sewage from the city of Ensenada (Segovia-Zavala et al 1988), runoff during the rainy season, debris from tuna farms, and oyster and mussel cultures. Altogether they contribute to maintain DIP and DIN at non-limiting concentrations for the development of blooms.…”
Section: Discussionmentioning
confidence: 99%
“…Existen diferentes fuentes locales de DIP y DIN en la BTS: agua de surgencias costeras transportadas al interior de la bahía (Espinosa-Carreón et al 2001, Segovia-Zavala et al 2007; aguas residuales vertidas desde la ciudad de Ensenada (Segovia-Zavala et al 1988); escorrentías durante la temporada de lluvias; desechos de las granjas de atún, así como los cultivos de mejillón y ostión. En conjunto estos flujos contribuyen a mantener altas concentraciones de DIN y DIP, por lo que en consecuencia no existen limitaciones de estos recursos para el desarrollo de los florecimientos.…”
Section: Discussionunclassified