Eddy properties in the Subtropical Countercurrent, Western Philippine Sea
Date of Original Version
An array of six oceanographic moorings with acoustic and environmental sensors was deployed in the central Philippine Sea from April 2010 to April 2011. The location spanned 18−23°N, 124 – 130°E in the Subtropical Countercurrent (STCC). The most prominent feature of the data set was a densely-packed eddy field with about equal numbers of cyclones and anticyclones moving westward at 6–12 km d−1. Eddies of either sign displaced the thermocline about ±50 m and had surface velocities exceeding 110 cm s−1. While warm eddies were slightly larger than cold eddies, the distance to maximum radial velocity was similar for both at about 65 km, close to the local Rossby radius of deformation. The steepness parameter U/c in the eddies ranged from 3 to 10, accompanied by relative vorticity of order 0.1–0.3 f, suggesting nonlinear, quasigeostrophic features with trapped cores rather than linear waves. This was borne out by the water mass analysis which showed high salinity, high spice North Pacific Tropical Water (NPTW) being transported westward in the warm eddy cores. The total KE and APE in eddies of both signs was about 1×1015 J with 85% of the APE and 74% of the KE located above 250 m depth. This equipartitioning of energy suggests mature eddies near equilibrium, that had been evolving for some time as they propagated into the area from the east.
Deep-Sea Research Part I: Oceanographic Research Papers
Ramp, S. R., J. A. Colosi, P. F. Worcester, F. L. Bahr, K. D. Heaney, J. A. Mercer, and L. J. Van Uffelen. "Eddy properties in the Subtropical Countercurrent, Western Philippine Sea." Deep-Sea Research Part I: Oceanographic Research Papers 125, (2017): 11-25. doi:10.1016/j.dsr.2017.03.010.