http://www.cnr.it/ontology/cnr/individuo/prodotto/ID45321
Dynamics of wind-forced coherent anticyclones in the open ocean (Articolo in rivista)
- Type
- Label
- Dynamics of wind-forced coherent anticyclones in the open ocean (Articolo in rivista) (literal)
- Anno
- 2009-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1029/2009JC005388 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Koszalka I; Bracco A; McWiliams JC; Provenzale A (literal)
- Pagina inizio
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://www.agu.org/pubs/crossref/2009/2009JC005388.shtml (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Koszalka, Provenzale: ISAC-CNR, Corso Fiume 4, Torino, Italy
Bracco: School of Earth and Atmospheric Science and Center for Nonlinear Science, Georgia Institute of Technology, Atlanta, Georgia, USA
McWilliams: Institute of Geophysics and Planetary Physics and Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, California, USA (literal)
- Titolo
- Dynamics of wind-forced coherent anticyclones in the open ocean (literal)
- Abstract
- We numerically study the dynamics of coherent anticyclonic eddies in the ocean
interior. For the hydrostatic, rotating, stably stratified turbulence we use a high-resolution
primitive equation model forced by small-scale winds in an idealized configuration. Many
properties of the horizontal motions are found to be similar to those of two-dimensional
and quasi-geostrophic turbulence. Major differences are a strong cyclone-anticyclone
asymmetry linked to the straining field exerted by vortex Rossby waves, which is also
found in shallow water flows, and the complex structure of the vertical velocity field,
which we analyze in detail. Locally, the motion can become strongly ageostrophic, and
vertical velocities associated with vortices can reach magnitudes and levels of spatial
complexity akin to those reported for frontal regions. Transport and mixing properties of
the flow field are further investigated by analyzing Lagrangian trajectories. Particles
released in the pycnocline undergo large vertical excursions because of the vertical
velocities associated to the vortices, with potentially important consequences for marine
ecosystem dynamics. (literal)
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