Record Details

Seasonal variability of alongshore geostrophic velocity off central California

ScholarsArchive at Oregon State University

Field Value
Title Seasonal variability of alongshore geostrophic velocity off central California
Names Chelton, Dudley B. (creator)
Date Issued 1984-05-20 (iso8601)
Note Copyrighted by American Geophysical Union.
Abstract Seasonal variability of alongshore geostrophic velocity relative to 500 dbar is examined from 23 years
of hydrographic data along two sections off central California (one off Point Sur and the other off Point
Conception). The seasonal cycles are determined by least square fits of the gappy data records to
harmonics with annual and semiannual periods. Attention is focused on variability over the outer
continental slope. Geostrophic flow in the upper 100 m along both sections is coherent and predominantly
annual with equatorward flow From February to September and poleward flow from October to
January. The flow deeper than 100 m is distinctly different along the two sections. The nearshore deep
flow is predominantly semiannual off Point Conception (notably different from surface flow) and poleward
all year with maxima in December and June. This semiannual variability at depth is a prevalent
feature of the California Current system. The nearshore deep flow off Point Sur is unusual in that it is
predominantly annual with maximum poleward flow in December and weak equatorward flow from
March to May. The seasonal variations over the continental slope compare favorably with existing
models of eastern boundary current systems in two respects: (1) The surface flow leads the predominantly
annual wind forcing in this region by about one month; and (2) the deep poleward counterfiow is
coherent with the local poleward barotropic pressure gradient at both locations, with a phase lag of
approximately 2 months. However, contrary to the results of existing dynamical models, the semiannual
poleward pressure gradient and undercurrent off Point Conception appear to be unrelated to the wind
forcing, which is predominantly annual in this region. These semiannual variations are highly coupled to
the semiannual flow throughout the water column inside the Southern California Bight, suggesting that
they may be topographically generated.
Genre Article
Identifier Chelton, D. (1984), Seasonal Variability of Alongshore Geostrophic Velocity Off Central California, J. Geophys. Res., 89(C3), 3473-3486.

© Western Waters Digital Library - GWLA member projects - Designed by the J. Willard Marriott Library - Hosted by Oregon State University Libraries and Press