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Wind-driven inner-shelf circulation off central Oregon during summer

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Title Wind-driven inner-shelf circulation off central Oregon during summer
Names Kirincich, Anthony R. (creator)
Barth, John A. (creator)
Grantham, Brian A. (creator)
Menge, Bruce A. (creator)
Lubchenco, Jane (creator)
Date Issued 2005 (iso8601)
Note copyrighted by American Geophysical Union
Abstract Velocity measurements from 17 deployments of moored acoustic Doppler current
profilers obtained during four summer upwelling seasons are used to describe the crossshelf
divergence of Ekman transport in the inner shelf off Oregon. For each deployment
the measured surface and bottom cross-shelf transports were compared with estimates
of the theoretical Ekman transports to find the fraction of full theoretical Ekman transport
present. In general, in 15 m of water at 1–2 km offshore, measured transport was 25% of
the full Ekman transport. Measured transports reached full Ekman transport 5–6 km
offshore in 50 m of water. This result indicates that the region of active upwelling marked
by the divergence of Ekman transport was limited to a narrow region along the coast. With
small wind stress curl and no major headlands in the region, no along-shelf trends
in the transport fractions were observed. Average transport fractions at each station were
similar from year to year with one exception. The interannual variability seen at this
particular site was most likely a result of local along-shelf bathymetric features. In
addition, a weak linear relationship was found between the ambient stratification and the
fraction of full Ekman transport. Reduced cross-shelf transport occurred at times of
decreased stratification. This type of ‘‘shutdown’’ of the inner-shelf cross-shelf circulation
has significant biological implications, sequestering production in the nearshore and
reducing larval cross-shelf transport.
Genre Article
Identifier Kirincich, A. R., Barth, J. A. , Grantham, B. A., Menge, B. A. and Lubchenco, J., 2005, Wind-driven inner-shelf circulation off central Oregon during summer: J. Geophys. Res., v. 110(C10), C10S03.

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