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A Compilation and Archive of Hydrographic Sections Across the Gulf Stream

A Compilation and Archive of Hydrographic Sections Across the Gulf Stream PDF Author: Paul Mazzarelli
Publisher:
ISBN:
Category : Gulf Stream
Languages : en
Pages : 78

Book Description

A Compilation and Archive of Hydrographic Sections Across the Gulf Stream

A Compilation and Archive of Hydrographic Sections Across the Gulf Stream PDF Author: Paul Mazzarelli
Publisher:
ISBN:
Category : Gulf Stream
Languages : en
Pages : 78

Book Description

Technical Series - Intergovernmental Oceanographic Commission

Technical Series - Intergovernmental Oceanographic Commission PDF Author: Intergovernmental Oceanographic Commission
Publisher:
ISBN:
Category : Oceanography
Languages : en
Pages : 278

Book Description

United States Hydrographic Office Manuscript Charts in the National Archives, 1838-1908

United States Hydrographic Office Manuscript Charts in the National Archives, 1838-1908 PDF Author: United States. National Archives and Records Service
Publisher:
ISBN:
Category : Nautical charts
Languages : en
Pages : 276

Book Description

Journal of Physical Oceanography

Journal of Physical Oceanography PDF Author:
Publisher:
ISBN:
Category : Marine meteorology
Languages : en
Pages : 742

Book Description

Time Series of Ocean Measurements

Time Series of Ocean Measurements PDF Author:
Publisher:
ISBN:
Category : Marine meteorology
Languages : en
Pages : 64

Book Description

Preliminary Results on Normalization of Hydrographic Sections of the Gulf Stream

Preliminary Results on Normalization of Hydrographic Sections of the Gulf Stream PDF Author: Timothy W. Kao
Publisher:
ISBN:
Category :
Languages : en
Pages : 6

Book Description
In this paper, we present the preliminary results of the normalization of the cross-stream density data compiled from three transects (Sections I, II, and III) of the Gulf Stream '60 data (Fuglister, 1963). All three sections are approximately perpendicular to the Stream direction. The procedure for the analysis is as follows: from the computed density field, we calculate first the sea-surface height anomaly across the front using 1500 m as the reference level. From the sea-surface height profile, we then estimate the value of the maximum slope of the profile and the maximum height change across the anomaly. From these, the length scale is readily obtained.

Transport Float Measurements and Hydrographic Station Data from Three Sections Across the Gulf Stream Near 67W̊

Transport Float Measurements and Hydrographic Station Data from Three Sections Across the Gulf Stream Near 67W̊ PDF Author: Joseph R. Barrett
Publisher:
ISBN:
Category : Ocean currents
Languages : en
Pages :

Book Description

Report of the Superintendent of the U.S. Coast and Geodetic Survey Showing the Progress of the Work During the Fiscal Year Ending with ...

Report of the Superintendent of the U.S. Coast and Geodetic Survey Showing the Progress of the Work During the Fiscal Year Ending with ... PDF Author: U.S. Coast and Geodetic Survey
Publisher:
ISBN:
Category : Coasts
Languages : en
Pages : 836

Book Description

Senate documents

Senate documents PDF Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 392

Book Description

Transport Float Measurements and Hydrographic Station Data from Three Sections Across the Gulf Stream Near 67 Degrees W R.V. CRAWFORD Cruise 168, June-July 1968

Transport Float Measurements and Hydrographic Station Data from Three Sections Across the Gulf Stream Near 67 Degrees W R.V. CRAWFORD Cruise 168, June-July 1968 PDF Author: Joseph Barrett
Publisher:
ISBN:
Category :
Languages : en
Pages : 96

Book Description
Three transects of the Gulf Stream between Cape Cod and Bermuda including data from transport float (free fall instrument) observations and hydrographic stations are presented and compared. Measured volume transport (by transport float observations) appeared to decrease from 180 plus or minus 20 to 113 plus or minus 20 million cu m/sec in a period of less than one week. Geostrophic calculations based on a reference level at the ocean bottom gave a volume transport of 100 to 120 million cu m/sec. Although the Stream appeared to extend to the ocean bottom on all three sections, deep countercurrents (westward flow) were also observed on two of the sections. (Author).
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