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dc.contributor.authorCollins, Curtis A.
dc.contributor.authorGarfield, Newell
dc.contributor.authorPaquette, Robert G.
dc.contributor.authorCarter, Everett
dc.date.accessioned2015-08-03T22:20:47Z
dc.date.available2015-08-03T22:20:47Z
dc.date.issued1996-09-01
dc.identifier.citationGeophysical Research Letters, Vol. 23, No. 18, pp. 2461-2464, September 1, 1996en_US
dc.identifier.urihttp://hdl.handle.net/10945/45730
dc.description.abstractSubsurface Lagrangian measurements at about 140 m showed that the path of the California Undercurrent lay next to the continental slope between San Francisco (37.80N) and St. George Reef (41.8øN) during mid-summer 1993. The mean speed along this 500k m path was 8 cm-s1 . The flow at this depth was not disturbed by upwelling centers at Point Reyes or Cape Mendocino. Results also demonstrate the ability to acoustically track floats located well above the sound channel axis along the California coast.en_US
dc.description.sponsorshipThis research was supported by the Naval Postgraduate School, the Office of Naval Research, and the Oceanographer of the Navy.en_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. As such, it is in the public domain, and under the provisions of Title 17, United States Code, Section 105, may not be copyrighted.en_US
dc.titleLagrangian Measurement of subsurface poleward Flow between 38 degrees N and 43 degrees N along the West Coast of the United States during Summer, 1993en_US
dc.typeArticleen_US
dc.contributor.departmentOceanographyen_US


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