Hydrographic station data obtained in the vicinity of Georges Bank, May and August, 1976
Citable URI
https://hdl.handle.net/1912/7731Location
Georges BankGulf of Maine
DOI
10.1575/1912/7731Keyword
Hydrography; Ocean temperature; Salinity; Eastward (Ship) Cruise E2B76; Oceanus (Ship : 1975-) Cruise OC13Abstract
Two extended cruises were made during May and August,
1976, to measure the regional hydrographic structure in
the vicinity of Georges Bank on the New England Continental
Shelf. A summary of the hydrographic observations made
during Cruise E2B76 on the R/V Eastward and leg 3 of
Cruise 13 on the R/V Oceanus are presented in graphic form.
Collections
Suggested Citation
Technical Report: Limeburner, Richard, Vermersch, John A., Beardsley, Robert C., "Hydrographic station data obtained in the vicinity of Georges Bank, May and August, 1976", 1978-08, DOI:10.1575/1912/7731, https://hdl.handle.net/1912/7731Related items
Showing items related by title, author, creator and subject.
-
Spatial variability of bottom turbulence over a linear sand ridge mooring deployment and AUTOSUB AUV survey cruise report R/V RRS Challenger, cruise number 146 Broken Bank, North Sea, U.K., 17 – 28 August 1999 cruise report
(Woods Hole Oceanographic Institution, 2001-08)Two successful AUTOSUB deployments were carried out during August 1999 as part of the AUTOSUB Thematic Program project titled “Spatial Variability of Bottom Turbulence over a Linear Sand Ridge,” funded by the Natural ... -
The Subduction experiment : cruise report RRS Charles Darwin cruise number 73 subduction 3 mooring deployment and recovery cruise, 30 September-26 October 1992
(Woods Hole Oceanographic Institution, 1993-03)Subduction is the mechanism by which water masses formed in the mixed layer and near the surface of the ocean find their way into the upper thermocline. The subduction process and its underlying mechanisms were studied ... -
The Subduction experiment : cruise report R/V Oceanus : cruise number 240 leg 3 : subduction 1 mooring deployment cruise, 17 June-5 July 1991
(Woods Hole Oceanographic Institution, 1993-03)Subduction is the mechanism by which water masses formed in the mixed layer and near the surface of the ocean find their way into the upper thermocline. The subduction process and its underlying mechanisms were studied ...
