Hostname: page-component-848d4c4894-4hhp2 Total loading time: 0 Render date: 2024-05-12T14:41:33.709Z Has data issue: false hasContentIssue false
  • English
  • Français

33.—A Review of the Branching of the Gulf Stream System*

Published online by Cambridge University Press:  05 December 2011

C. R. Mann
Get access

Synopsis

The surveys of temperature and salinity that have led to the concept that the Gulf Stream splits into branches are reviewed, beginning with the survey made by Helland-Hansen on board the Michael Sars in 1910. The system of currents, or branches, between the Newfoundland Banks and the Mid- Atlantic deduced by the different investigations from charts of temperature, or by dynamic computation, are not all compatible. There is good evidence that part of the Gulf Stream turns south-east after passing the Newfoundland Banks and part turns north to become the North Atlantic Current. Both these currents are boundaries between water masses in the upper layer of the ocean. The evidence for permanent currents other than these two is conflicting.

Type
Ocean Circulation
Information
Proceedings of the Royal Society of Edinburgh, Section B: Biological Sciences , Volume 72 , Issue 1 , 1972 , pp. 341 - 349
Copyright
Copyright © Royal Society of Edinburgh 1972

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

References To Literature

Dietrich, G., 1964. Oceanic Polar Front Survey in the North Atlantic. Res. Geophys., 291–308.Google Scholar
Fuglister, F. G., 1951. Multiple currents in the Gulf Stream System. Tellus, 3, 230–233.CrossRefGoogle Scholar
Fuglister, F. G., 1963. Gulf Stream '60. Prog. Oceanogr., 1, 265–373.CrossRefGoogle Scholar
Fuglister, F. G. and Worthington, L. V., 1951. Some results of a multiple ship survey of the Gulf Stream. Tellus, 3, 1–14.CrossRefGoogle Scholar
Helland-Hansen, B., 1912. In The Depths of the Ocean (Murray, J. and Hjort, J.), 210–306. London.Google Scholar
Helland-Hansen, B. and Nansen, F., 1926. The Eastern North Atlantic. Geofys. Publr, 4, (2), 1–74.Google Scholar
Iselin, C. O'D., 1936. A Study of the circulation of the Western North Atlantic. Pap. Phys. Oceanogr. Met., 4, 1–101.Google Scholar
Mclellan, H. J., 1957. On the distinctness and origin of the Slope Water off the Scotian Shelf and its easterly flow south of the Grand Banks. J. Fish. Res. Bd Can., 14, 213–239.CrossRefGoogle Scholar
Mann, C. R., 1967. The termination of the Gulf Stream and the beginning of the North Atlantic Current. Deep Sea Res., 14, 337–359.Google Scholar
Worthington, L. V., 1962. Evidence for a two gyre circulation system in the North Atlantic. Deep Sea Res., 9, 51–67.Google Scholar