2006
DOI: 10.1016/j.pocean.2006.03.005
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A review of eastern tropical Pacific oceanography: Summary

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Cited by 73 publications
(56 citation statements)
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References 30 publications
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“…Diversity patterns of bycatch assemblages in both fishing modes in the eastern tropical Pacific match reasonably well with the principal characteristics of its oceanography, hydrography and circulation (Fiedler and Talley, 2006;Kessler, 2006;Lavín et al, 2006;Pennington et al, 2006). In the case of the environmental variables, the sea surface temperature and chlorophyll were the environment predictors that better explained diversity patterns (Table 3).…”
Section: Geographical and Habitat Characteristics Of Bycatch Assemblagessupporting
confidence: 59%
“…Diversity patterns of bycatch assemblages in both fishing modes in the eastern tropical Pacific match reasonably well with the principal characteristics of its oceanography, hydrography and circulation (Fiedler and Talley, 2006;Kessler, 2006;Lavín et al, 2006;Pennington et al, 2006). In the case of the environmental variables, the sea surface temperature and chlorophyll were the environment predictors that better explained diversity patterns (Table 3).…”
Section: Geographical and Habitat Characteristics Of Bycatch Assemblagessupporting
confidence: 59%
“…The ETNP ODZ comprises part of the North Pacific subtropical gyre; specifically, it is delimited southeastern by the California Current (CC), the North Equatorial Current (NEC) and the North Equatorial Countercurrent (NECC) (Karstensen et al, 2008). The boundary area where the CC, flowing along the coast of the Baja California and northern Mexico, encounters the NEC is characterized by Ekman transport westward and upwelling mainly off the Californian coast and in a weakened magnitude off the northern Mexico coast (Kessler, 2006;Lavín et al, 2006). Our sampling area lies in this transition region; however the upper water circulation in this region is not yet fully understood (Kessler, 2006).…”
Section: Environmental Setting Of the Etnpmentioning
confidence: 99%
“…Por el contrario, Giraldo, et al [5] plantean que este enfriamiento estacional es consecuencia de la respuesta oceánica a un forzante atmosférico del POT. En el sector oriental del Océano Pacífico han sido descritos tres forzantes atmosféricos principales: el chorro de viento de Panamá (diciembre abril), el chorro de viento del Chocó (octubre -noviembre) y el cinturón de convergencia intertropical (19)(20)(21). Cuando los vientos Alisios del norte se intensifican, el chorro de viento de Panamá afecta drásticamente la capa de influencia friccional del Panama Bight, provocando una consecuente respuesta oceánica en forma de una extensa lengua de surgencia que puede extenderse desde los 7º N hasta la zona ecuatorial [6,7,22].…”
Section: Giraldo:variabilidad Termohalina En El Pnn Gorgonaunclassified