Penven Pierrick, Echevin V., Pasapera J., Colas F., Tam J. (2005). Average circulation, seasonal cycle, and mesoscale dynamics of the Peru current system : a modeling approach - art. no. C10021. Journal of Geophysical Research Oceans, 110 (C10), p. NIL_67-NIL_87. ISSN 0148-0227.
Titre du document
Average circulation, seasonal cycle, and mesoscale dynamics of the Peru current system : a modeling approach - art. no. C10021
Penven Pierrick, Echevin V., Pasapera J., Colas F., Tam J.
Source
Journal of Geophysical Research Oceans, 2005,
110 (C10), p. NIL_67-NIL_87 ISSN 0148-0227
[1] The Humboldt Current System is the most productive of the eastern boundary currents. In the northern part, the Peru Current System (PCS) is located between 5 degrees S and 20 degrees S. Along the Peruvian coast, an equatorward wind forces a strong coastal upwelling. A high resolution model is designed to investigate the mean circulation, the seasonal cycle, and the mesoscale dynamics for the PCS. The model is able to reproduce the equatorward Peru Coastal Current (PCC), the Peru Chile Under-Current (PCUC) which follows the shelf break towards the pole, and the Peru-Chile Counter-Current (PCCC) which flows directly towards the south and veers to the west around 15 degrees S. While the upper part of the PCUC is close to the surface and might even outcrop as a counter current, the bottom part follows f/H isolines. The PCCC appears to be directly forced by the cyclonic wind stress curl. The model is able to produce the upwelling front, the cold water tongue which extends toward the equator and the equatorial front as described in the literature. Model seasonal changes in SST and SSH are compared to measurements. For the central PCS, model EKE is 10% to 30% lower than the observations. The model eddy diameters follow a strong equatorward increase. The injection length scales, derived from the energy spectra, strongly correlate to the Rossby radius of deformation, confirming the predominant role of baroclinic instability. At 3 degrees S, the model solution appears to switch from a turbulent oceanic regime to an equatorial regime dominated by zonal currents.
