Antarctic Science

  • Antarctic Science (2009), 21 : pp 135-148
  • Copyright © Antarctic Science Ltd 2009
  • DOI: 10.1017/S0954102008001636 (About DOI)
  • Published online: 19 November 2008
Cambridge Journals Online - CUP Full-Text Page
Antarctic Science (2009), 21:135-148 Cambridge University Press
Copyright © Antarctic Science Ltd 2009
doi:10.1017/S0954102008001636

Biological Sciences

ENSO and variability of the Antarctic Peninsula pelagic marine ecosystem


Valerie J. Loeba1 c1, Eileen E. Hofmanna2, John M. Klincka2, Osmund Holm-Hansena3 and Warren B. Whitea3

a1 Moss Landing Marine Laboratories, 8272 Moss Landing Road, Moss Landing, CA 95039, USA
a2 Center for Coastal Physical Oceanography, Old Dominion University, Norfolk, VA 23529, USA
a3 Scripps Institution of Oceanography, La Jolla, CA 92093, USA
Article author query
loeb vj [PubMed]  [Google Scholar]
hofmann ee [PubMed]  [Google Scholar]
klinck jm [PubMed]  [Google Scholar]
holm-hansen o [PubMed]  [Google Scholar]
white wb [PubMed]  [Google Scholar]

Abstract

The West Antarctic Peninsula region is an important source of Antarctic krill (Euphausia superba) in the Southern Ocean. From 1980–2004 abundance and concentration of phytoplankton and zooplankton, krill reproductive and recruitment success and seasonal sea ice extent here were significantly correlated with the atmospheric Southern Oscillation Index and exhibited three- to five-year frequencies characteristic of El Niño–Southern Oscillation (ENSO) variability. This linkage was associated with movements of the Southern Antarctic Circumpolar Current Front and Boundary, a changing influence of Antarctic Circumpolar Current and Weddell Sea waters, and eastward versus westward flow and mixing processes that are consistent with forcing by the Antarctic Dipole high-latitude climate mode. Identification of hydrographic processes underlying ecosystem variability presented here were derived primarily from multi-disciplinary data collected during 1990–2004, a period with relatively stable year-to-year sea ice conditions. These results differ from the overwhelming importance of seasonal sea ice development previously established using 1980–1996 data, a period marked by a major decrease in sea ice from the Antarctic Peninsula region in the late 1980s. These newer results reveal the more subtle consequences of ENSO variability on biological responses. They highlight the necessity of internally consistent long-term multidisciplinary datasets for understanding ecosystem variability and ultimately for establishing well-founded ecosystem management. Furthermore, natural environmental variability associated with interannual- and decadal-scale changes in ENSO forcing must be considered when assessing impacts of climate warming in the Antarctic Peninsula–Weddell Sea region.

(Received July 17 2007)

(Accepted August 19 2008)

Key wordsAntarctic Circumpolar Current; Antarctic Dipole; atmospheric-oceanic coupled processes; climate regime shifts; Euphausia superba; Southern Ocean

Correspondence:

c1 loeb@mlml.calstate.edu


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