SciELO - Scientific Electronic Library Online

vol.42 número4Origen del Alineamiento Submarino de Pascua: morfología y lineamientos estructuralesRemolinos intratermoclina en el Archipiélago Juan Fernández, Océano Pacífico suroriental índice de autoresíndice de assuntospesquisa de artigos
Home Pagelista alfabética de periódicos  

Serviços Personalizados




Links relacionados

  • Em processo de indexaçãoCitado por Google
  • Não possue artigos similaresSimilares em SciELO
  • Em processo de indexaçãoSimilares em Google


Latin american journal of aquatic research

versão On-line ISSN 0718-560X


ANDRADE, Isabel; HORMAZABAL, Samuel  e  CORREA-RAMIREZ, Marco. Time-space variability of satellite chlorophyll-α in the Easter Island Province, southeastern Pacific Ocean. Lat. Am. J. Aquat. Res. [online]. 2014, vol.42, n.4, pp.871-887. ISSN 0718-560X.

The Easter Island Province (EIP) encompasses Easter Island (EI) and Salas y Gómez Island (SGI), which are located in the eastern boundary of the south Pacific subtropical gyre. This province is one of the most oligotrophic region in the world ocean with a high degree of endemism and distinguished by having the clearest waters in the world. Issues related to the biophysical coupling that sustains biological production in this region are still poorly understood. Satellite data compiled over a ten year period was used to characterize the spatial and temporal chlorophyll-α (Chl-α) variability around the EIP and determine the relationship between Chl-α and several physical forcing. Results shows a clear Chl-α annual cycle around the EIP, with maximum concentration during the austral winter. Chl-α spatial distribution shows a strong zonal dipole over EI that divides the island into two zones: southeast and northwest. Due to its small size and low elevation of SGI, it does not generate a significant local effect in Chl-α concentration, but a Chl-α increase is observed southeast of this island (~2 km) associated to a seamount. The mean geostrophic current in the EIP flows eastward, associated with the southeastern boundary of the subtropical gyre. However, recurrent mesoscale eddies traveling northwestward and produce large surface current variability with periods of high velocities in opposite direction. In the spring, wakes of high Chl-α concentration can be observed over EI, associated with the generation and detachment of submesoscale eddies from EI, which could have important biological implications during periods of low regional biological production.

Palavras-chave : satellite chlorophyll-α; mesoscale and submesoscale eddies; subtropical anticyclonic gyre; Easter Island; Salas y Gómez Island; southeastern Pacific.

        · resumo em Espanhol     · texto em Inglês     · Inglês ( pdf )


Creative Commons License Todo o conteúdo deste periódico, exceto onde está identificado, está licenciado sob uma Licença Creative Commons