Revised August 1977. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the Sea Grant Catalog: http://seagrant.oregonstate.edu/publications
Published October 1968. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the Sea Grant Catalog: http://seagrant.oregonstate.edu/publications
Revised October 1972. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the Sea Grant Catalog: http://seagrant.oregonstate.edu/publications
CTD observations were made along sections near Coos Bay at 43° 13'N, off Crescent City at 41° 54'N, off Eureka at 40° 51 'N, off of Half Moon Bay at 37°2q'N, off of Pt. Purisima at 34° 45'N, and along the Code Central and Pt. Arena lines near 39°N during...
CTD observations were made in the Code region near Pt. Arena on the
northern California coast at 39°N, off Coos Bay at 43°12'N, off Crescent
City at 41°54'N, of Eureka at 40°51'N, off Half Moon Bay at 37°25'N, off
Pt. Purisima at 34°45'N and in the Santa Barbara Channel during...
Current meter moorings were recovered and deployed off of Coos Bay at 43°13'N, off of Crescent City at 41°54'N, off of Half Moon Bay at 37°25'N and off of Pt. Purisima at 34°45'N during 28-29 January 1982. CTD observations were made off of Coos Bay at 43°13 1 N, off...
CTD observations were made in the CODE region near Pt. Arena on the northern California coast at 39°N, off Coos Bay, Oregon at 43°13'N, off Crescent City at 41°541N, and off Half Moon Bay at 37°25'N. The observations in the CODE region included two repeated sections along the Central Line,...
Influences of tidal and slower (subtidal) oceanic flows over the continental shelf and slope off Oregon are studied using a high-resolution ocean circulation model and comparative model-data analyses. The model is based on the Regional Ocean Modeling System (ROMS), a fully nonlinear, three-dimensional model (using hydrostatic and Boussinesq approximations). The...
Inner-shelf circulation and mechanisms of across-shelf transport of water masses were examined using seven years of observations collected by the Partnership for Interdisciplinary Studies of Coastal Oceans (PISCO) program, a long-term monitoring effort along the central Oregon coast. Since 1998, moored velocity and hydrographic measurements have been obtained during the...
Analogous to ocean surface waves, waves in the ocean interior also experience steepening, breaking, and dissipation as they approach the coastline. Much less is known about this internal beach. In this work, extensive moored Acoustic Doppler Current Profiler and temperature/salinity data together with optical remote sensing are combined to describe...