Wind stress forcing of the Oregon coastal ocean during the 1999 upwelling season

Journal of Geophysical Research: Oceans

Volumn 107, Issue 5, 2002, Pages

  Samelson, R ^a   Barbour, P ^a   Barth, J ^a   Bielli, S ^a   Boyd, T ^a   Chelton, D ^a   Kosro, P ^a   Levine, M ^a   Skyllingstad, E ^a   Wilczak, J ^a  

^a OREGON STATE UNIVERSITY   (United States)

Author keywords

Air sea coupling; Coastal meteorology; Coastal upwelling; Marine atmospheric boundary layer; Mesoscale modeling; Remote sensing

Indexed keywords

AIR-SEA INTERACTION; COASTAL CIRCULATION; MODELING; REMOTE SENSING; UPWELLING; WIND FORCING;

OREGON; UNITED STATES;

EID: 0037096011     PISSN: None     EISSN: 21699291     Source Type: Journal    
DOI: None     Document Type: Article

References (17)

1. Models of wind-driven currents on the continental shelf
2. Separation of a coastal upwelling jet at Cape Blanco, Oregon, USA
3. A separating coastal upwelling jet at Cape Blanco, Oregon, and its connection to the California current system
4. Local atmospheric forcing during the coastal ocean dynamics experiments 1 and 2, 1, A description of the marine boundary layer and atmospheric conditions over a northern California upwelling region
5. The diurnal cycle along the Oregon coast during summertime
6. The new NMC mesoscale eta model: Description and forecast examples
7. The summertime low-level jet and marine boundary layer structure along the California coast
8. The hydraulics of an evolving upwelling jet flowing around a cape
9. The accuracy of the NSCAT-1 vector winds: Comparisons with national data buoy center buoys
10. The large-scale coastal wind field along the west coast of North America, 1981 - 1982
11. Open ocean momentum flux measurements in moderate to strong winds
12. Spaceborne radar measurement of wind velocity over the ocean - An overview of the NSCAT scatterometer system
13. Assimilation of surface velocity data into a primitive equation coastal ocean model
14. Supercritical marine-layer flow along a smoothly varying coastline
15. The horizontal momentum balance in the marine atmospheric boundary layer during CODE-2
16. The marine layer off northern California: An example of supercritical channel flow