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Phillips, Norman A. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
A graph of the latitude of jet streams at 80° W longitude for a 49-day period in the winter of 1947–8 shows that the jet stream undergoes changes which appear as discontinuities on such a graph. Several cases are discussed which illustrate the manner in which these discontinuities appear. The new jets so formed then appear to experience a southward displacement before their disappearance. Accompanying the southward displacement at this longitude is a disappearance of the solenoidal field accompanying the jet in the lower troposphere, and an increase of the potential temperature in the center of the jet.DOI: 10.1111/j.2153-3490.1950.tb00320.x
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    • BERGGRENR,., B. BOLIN and C.-G. ROSSBY1,949: An aerological Study of Zonal Motion, its Perturbations and Breakdown. Tdlus, I , 2, pp. 14-37.
    • CRESSMANG,. P., 1950: Variations in the Structure of the Upper Westerlies. Joum. of, Mcr., 7, I , pp. 3 9-47.
    • HOVMOLLERE,., 1y48 : North-South Cross Sections showing Distributions of Temperature, Relative Humidity, and Wind in a Well-marked Zonal Current over Western Europe. J o u m . ofMet., s, 2 , pp. 67-69.
    • NAMIASJ,., and P. F. CLAPF,1949 : Confluence Theory of the High Tropospheric Jet Stream. Joum. of Met., 6 , 5. pp. 330-336.
    • P A L M ~EN.,, and C. W. NEWTON1,948: A Study of the Mean Wind and Temperature Distribution in the Vicinity of the Polar Front in Winter. Jourttnl qf Met., 5 , 5 , pp. 2 2 0 - 226.
    • RIEHL, H., 1948 : Jet Stream in Upper Troposphere and Cyclone Formation. Trariz..Amer. Geophyx. U n i o n , 2 9 , 2, pp. 175-186.
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  • BioEntity Site Name
    1y48Protein Data Bank

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