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Intrathermocline eddies in the coastal transition zone off central Chile (31–41°S)

ScholarsArchive at Oregon State University

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Title Intrathermocline eddies in the coastal transition zone off central Chile (31–41°S)
Names Hormazabal, Samuel (creator)
Combes, Vincent (creator)
Morales, Carmen E. (creator)
Correa-Ramirez, Marco A. (creator)
Di Lorenzo, Emmanuel (creator)
Nuñez, Sergio (creator)
Date Issued 2013-10-02 (iso8601)
Note This is the publisher’s final pdf. The published article is copyrighted by the American Geophysical Union and can be found at: http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)2169-9291.
Abstract The three-dimensional structure and the origin of mesoscale anticyclonic
intrathermocline eddies (ITEs) in the coastal transition zone (CTZ) off central Chile (31–41°S) were analyzed through the combination of data from oceanographic cruises and
satellite altimetry, and the application of an eddy-resolving primitive equation ocean model
coupled with a numerical experiment using a passive tracer. In this region, ITEs are
represented by subsurface lenses (~100 km diameter; 500 m thickness or vertical
extension) of nearly homogeneous salinity (>34.5) and oxygen-deficient (<1.0 mL L⁻¹)
waters, properties which are linked to the equatorial subsurface water mass (ESSW)
transported poleward by the Peru-Chile undercurrent (PCUC) in the coastal band. At least
five to seven ITEs were observed simultaneously in the area between 31° and 38°S during
winter cruises in 1997 and 2009. Satellite data indicated that the ITEs identified from in situ
data moved westward, each at a mean speed of ~2 km d⁻¹ and transported a total volume
of ~1 x 10⁶ m³ s⁻¹ (=1 Sv); the lifespan of each ITE ranged from a few months to 1 year.
Model results indicate that ITEs become detached from the PCUC under summer upwelling
conditions in the coastal zone.
Genre Article
Topic Intrathermocline eddies
Identifier Hormazabal, S., V. Combes, C. E. Morales, M. A. Correa-Ramirez, E. Di Lorenzo, and S. Nuñez (2013), Intrathermocline eddies in the coastal transition zone off central Chile (31–41°S), Journal of Geophysical Research: Oceans, 118, 4811–4821. doi:10.1002/jgrc.20337

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