1995
DOI: 10.7773/cm.v21i2.987
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Short term variations of the anticyclonic circulation in Bahía Sebastián Vizcaíno, BC

Abstract: A partir de observaciones hidrográficas de corrientes e imágenes de satélite obtenidas del 7 al 19 de septiembre de 1992, se analiza la variabilidad en escala de tiempo de días de un giro anticiclónico localizado en bahía Sebastián Vizcaíno. Los resultados de este trabajo indican que durante septiembre de 1992 hubo una estrecha relación entre la manifestación superficial de un giro de agua cálida en el interior de bahía Sebastián Vizcaíno y la intensificación o relajamiento de la surgencia al norte de la bahía… Show more

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Cited by 8 publications
(6 citation statements)
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“…In comparison with all other sampling areas, the PB region is characterized by the occurrence of a strong coastal southward current 35 and eddies 26,32,48 . Such distinctive oceanographic features in this area allow year‐round upwelling, and high primary production (up to 8 mg/m 3 of chlorophyll‐a 33,48 ).…”
Section: Discussionmentioning
confidence: 95%
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“…In comparison with all other sampling areas, the PB region is characterized by the occurrence of a strong coastal southward current 35 and eddies 26,32,48 . Such distinctive oceanographic features in this area allow year‐round upwelling, and high primary production (up to 8 mg/m 3 of chlorophyll‐a 33,48 ).…”
Section: Discussionmentioning
confidence: 95%
“…Near the southern limit of the species, the PE sites showed a homogeneous haplotype frequency. This protruding point, the largest on the entire peninsula of Baja California, has connectivity with the California Current through the anticyclone eddy of San Sebastian in Vizcaino Bay 35 . This eddy brings large amounts of water from the north through the California Current.…”
Section: Discussionmentioning
confidence: 96%
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“…patterns that can lead to intense regional upwelling (Mancilla-Peraza et al 1993;Amador-Buenrostro et al 1995;Dailey et al 2021). However, the BSV ecosystem experiences weaker regional upwelling compared to the SCB, both due to BSV being located further south away from the California Current system as well as seasonal cyclonic circulation within the bay (Amador- Buenrostro et al 1995). These factors contribute to a decrease in upwelling intensity at times (Huyer 1983), which is not observed in the SCB.…”
Section: Chemical Variation Between Nursery Regionsmentioning
confidence: 99%