Variability of sea-floor roughness within the Coastal Ocean Dynamics Experiment (CODE) region
Citable URI
https://hdl.handle.net/1912/8902DOI
10.1575/1912/8902Keyword
Coastal Ocean Dynamics Experiment (CODE); Ocean waves; Ocean-atmosphere interaction; Ocean bottomAbstract
This report briefly summarizes the geological and biological data taken
oft northern California before and during the Coastal Ocean Dynamics
Experiment (CODE) (Allen et al, 1982) by the principal investigators of the
bottom stress/bottom boundary layer component of CODE (D. Cacchione, D. Drake,
USGS; and W. Grant, A. Williams, WHOI) and other cooperating investigators of
the U.S. Geological Survey.
Suggested Citation
Technical Report: Cacchione, David A., Drake, David E., Grant, William D., Williams, Albert J., Tate, George B., "Variability of sea-floor roughness within the Coastal Ocean Dynamics Experiment (CODE) region", 1983-06, DOI:10.1575/1912/8902, https://hdl.handle.net/1912/8902Related items
Showing items related by title, author, creator and subject.
-
A vector-averaging wind recorder (VWAR) system for surface meteorological measurements in CODE (Coastal Ocean Dynamics Experiment)
(Woods Hole Oceanographic Institution, 1988-05)As part of the Coastal Ocean Dynamics Experiment (CODE) field program, moored buoys were instrumented to measure and record wind speed and direction, air and water temperature, insolation, barometric pressure and relative ... -
Use of SF5CF3 for ocean tracer release experiments
(American Geophysical Union, 2008-02-19)SF6 tracer release experiments (TREs) have provided fundamental insights in many areas of Oceanography. Recently, SF6 has emerged as a powerful transient tracer, generating a need for an alternative tracer for large-scale ... -
Coastal mixing and optics experiment : mooring deployment cruise report R/V Oceanus cruise number 284 31 July-11 August 1996
(Woods Hole Oceanographic Institution, 1997-08)An array of moorings at four sites at a mid-shelf location in the mid-Atlantic Bight was deployed for a period of 10 months beginning in August 1996 as part of the Coastal Mixing and Optics Experiment (CMO), funded by the ...
