|
|
Coastal Upwelling Dynamics
Abstract:
Both theoretical method (Song et al. 2001a; Song and Chao 2002)
and modeling approach (Song et al. 2001b) have been used.
These recent studies reveal that the alongshore-varying
topography plays an important role in causing the meandering
upwelling fronts to break and form cold filaments.
For example, five cross-shore transport jets are determined along
the northern California region (Figure 2) and each carries 5 to
15 Sv of coastal water offshore. Such kinds of jets have
important implications for estimating coastal fluxes in global
biogeochemical studies. Future study will focus on assessing
the impact of the time-space variability of local and remote
forcing on the formation of coastal upwelling and frontal variability.
Figure 1:
Satellite image of SST shows multiple upwelling centers and cold
filaments off central California (Courtesy of E. Armstrong).
Figure 2:
Model results showing multiple cross-shore transport jets off the
US West coast (Song et al., 2001)
Reference:
Song, Y. T., D. Haidvogel, and S. Glenn, 2001a:
The effects of topographic variability on the formation
of upwelling centers off New Jersey: A theoretical model, J. Geophys. Res. 106, 9223-9240.
Song, Y. T., and Y. Chao, 2002: The role of topography in coastal upwelling
and cross-shore exchange: A theoretical study, Ocean Modeling, submitted.
Song, Y. T., Y. Chao, P. Marchesiello, and J. C. McWilliams, 2001b: The role of topography in coastal upwelling and cross-shore exchange: A computational study, J. Phys. Oceanogr., revised.
|

