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Dynamical analysis of the upwelling circulation off central Chile

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Title Dynamical analysis of the upwelling circulation off central Chile
Names Mesias, Jorge M. (creator)
Matano, Ricardo P. (creator)
Strub, P. Ted (creator)
Date Issued 2003 (iso8601)
Note copyrighted by American Geophysical Union
Abstract In this article we analyze the momentum and vorticity balances of a numerical
simulation of the upwelling circulation off central Chile (34° –40°S) and its response to
interannual local wind changes. Our analysis indicates that the path of the upwelling jet is
strongly controlled by the bottom topography. This topographic steering causes the jet to
separate from the coast at the Punta Lavapie cape (~37°S). Although the zeroth-order
momentum balance is dominated by the geostrophic terms, the circulation is also affected
by nonlinear processes, which lead to the formation of large meanders and the shedding of
cyclonic eddies north of Punta Lavapie during periods of wind relaxation. The relative
contributions of the zeroth-order vorticity balance and the advective terms are also strongly
controlled by changes in the coastline geometry and the bottom topography. Vorticity is
created along the current axes and transported toward the coast and the Peru-Chile Trench,
where it dissipates. South of Punta Lavapie the across-shelf transports are weaker with
equatorward flows that are more stable than in the north. Additional numerical simulations
indicate that during periods with El Niño conditions, the area is affected with a general
weakening of the currents and upwelling activity, although the northern region still shows
the formation of eddies. During years with relatively stronger winds, in contrast, the
upwelling activity and across-shelf transport processes are significantly increased. The
results show that the Punta Lavapie cape has a large effect on the spatial and temporal
variability of the coastal currents in the region off central Chile.
Genre Article
Identifier Mesias, J. M., Matano, R. P., Strub, P. T., Dynamic analysis of the upwelling circulation off central Chile, J. Geophys. Res., 108, C3.

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