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The evolving structure of an upwelling filament

Flament, Pierre, Armi, Laurence, Washburn, Libe·1985·Journal of Geophysical Research: Oceans

Abstract

The evolution of an upwelling filament was studied over a 2‐week period by using satellite infrared images, and its thermohaline structure was mapped in situ. The surface velocity field consisted of a large meander extending offshore for at least 300 km. The northern branch was ∼40 km wide, flowing offshore at a peak velocity of 0.55 m/s; the southern branch was flowing inshore at 0.35 m/s. The offshore transport was more than 10 6 m 3 s−1, larger than the Ekman transport. The meander was unstable to barotropic instabilities at a scale of ∼15 km. From a succession of images a surface convergence γ ≈ 8·10−6 s−1 over 20 km was observed near the sharp front limiting the filament to the south. The ∼350 m width of the front indicates a separation of scales between the large‐scale strain field and the mixed‐layer turbulence parameterized with an eddy diffusion coefficient KH ≈ 0.25 m 2 s−1. Thermohaline layers that originated at the convergence near the sharp front suggest a secondary circulation subducting denser waters to the south underneath the lighter northern water.

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Metadata

Authors
Flament, P., Armi, L., & Washburn, L.
Venue
Journal of Geophysical Research: Oceans
Published
1985-11-20
Volume
90
Issue
C6
Pages
11765-11778
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2039067330
Cited by
276
References
12
FWCI
9.71
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: The evolving structure of an upwelling filament. https://app.cochat.ai/papers/10.1029/jc090ic06p11765
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Flament, P., Armi, L., & Washburn, L. (1985). The evolving structure of an upwelling filament. Journal of Geophysical Research: Oceans. https://doi.org/10.1029/jc090ic06p11765

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