MOORED OBSERVATIONS OF THE CURRENT AND TEMPERATURE STRUCTURE OVER THECONTINENTAL-SLOPE OFF CENTRAL CALIFORNIA 2 - THE ENERGETICS OF THE FLOW OFF POINT SUR

The data from two current meter moorings off Point Sur, California, we re analyzed to examine the energy transfers over the continental slope in the California Current system (CCS). The method used was to calcul ate terms in the heat equation at intermediate depths between instrume nts, using the thermal wind relation to estimate the horizontal temper ature gradients from the vertical shear. Time series of u, v, and T we re collected for 17 months (May 1989 to October 1990) at site P2 on th e 800-m isobath and for 12 months (May 1990 to May 1991) at site P3, 2 5 km farther offshore on the 1800-m isobath. Instrument depths were 10 0, 350, and 500 m at both moorings plus 1000 m at site P3. Mean values of the energy conversion terms were computed at sites P2 and P3 at 22 5 m depth and at site P2 at 425 m depth. The local change of eddy pote ntial energy (EPE) was approximately balanced (partial derivative EPE/ partial derivative t approximate to 0) for each case but the dynamics were quite different. At P2 225, the sources of EPE were advection by the mean flow and baroclinic instability, which converted mean potenti al energy (MPE) to EPE. The losses came from eddy advection out of the region and the vertical eddy heat flux (VEHF), which converted EPE to eddy kinetic energy (EKE). At P2 425, baroclinic instability provided the major source of EPE. This, plus a small positive contribution fro m the VEHF, was balanced by advection of EPE out of the region by both the mean flow and the eddies. At P3 225, mean advection and baroclini c instability were negligible, and the downward eddy heat flux (VEHF) was balanced by advection of heat out of the region by the eddies. Tim e series of terms in the EPE equation were used to examine high energy transfer events at both moorings, Events at P2 involved both horizont al and vertical processes and had longer timescales (several days to w eeks) than those at P3, which had much shorter timescales (2-5 days) a nd were: dominated by vertical processes. Compared to the Gulf Stream, the mean baroclinic instability at P2 (both depths) was smaller by at least a factor of 10. A term-by-term comparison between the mean valu es off Point Sur and the Kuroshio Extension showed different processes , with the eddies gaining strength at the expense of the mean flow off Point Sur and the opposite occurring in the Kuroshio Extension.