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Fuglister, F. C. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
A new interpretation of the accumulated temperature and salinity data from the Gulf Stream Area indicates that the System is made up of a series of overlapping currents. These currents are separated by relatively weak countercurrents. Data from a recent survey are presented as supporting this hypothesis.DOI: 10.1111/j.2153-3490.1951.tb00804.x
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    • FUGLISTEFR., C., 1947: Average Monthly Sea Surface Temperatures of the Western North Atlantic Ocean. Papers i n Physical Oceanography and Meteorology, 10,2, pp. 1-25.
    • FUGLISTEFR., C., and L. V. WORTHINGT1O9N51,:Some Results of a Multiple Ship Survey of the Gulf Stream. Tellus, 3, I,pp. 1-14.
    • ISELIN,C. O'D., 1936: A Study of the Circulation of the Western North Atlantic. Papers in Physicil Oceanography and Meteorology, 4, 4, pp. 1-101.
    • - 1940: Preliminary Report on Long-Period Variations in the Transport of the Gulf Stream System, Papers in Physisical Oceanography and Meteorology, 8 , I, pp. 1-40.
    • ROSSBYC,.-G., 1936:Dynamics of Steady Ocean Currents in the Light of Experimental Fluid Mechanics. Papers in Physical Oceanography and Mefeorology, 5. I, pp. 1-26.
    • SVERDRUHP,. U., M. W. JOHNSON and R. H. FLEMING, 1942: The Oceans: Their Physics, Chemistry, and General Biology. New York, Prentice-Hall.
    • VON ARX,WILLIASM., 1950: An Electromagnetic Method for Measuring the Velocities of Ocean Currents from a Ship Under Way. P a p m in Physical Oceanography and Meteorology. 9, 3, pp. 1-26.
    • WUST, GEORG,and, ALBERTDEPANT,1936: Atlas zur Schichtung und Zirkulation des Atlantischen Ozeans. Deutsche Atlantische Expedition Meteor 1925-1927, Wiss. Erg., Bd. V1-Atlas, Berlin.
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