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Newell, Reginald E.; Vincent, Dayton G.; Kidson, John W. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Two mechanisms contribute to interhemispheric mass exchange: large scale eddy transfer and mean meridional circulations. Estimates of both are presented based on data from a recently completed study of the general circulation of the tropics. The long term interhemispheric exchange time is found to be about 320 days. It is suggested that when eddy processes reinforce the transfer by mean meridional circulations in the upper troposphere in late spring and summer much faster exchange rates may occur which may be responsible for an apparent anomaly in the seasonal variation of surface ozone in the southern hemisphere. Finally the interhemispheric mass flux is compared with a crude estimate of the tropospheric-stratospheric mass flux based on the same tropical data.DOI: 10.1111/j.2153-3490.1969.tb00471.x
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    • Aldaz, L. 1965. Atmospheric ozone in Antarctica. tion provided by the measurements of helium J. Geophys. Res., 70, 1767-1773. and water vapour distribution in the stratosphere.
    • Bolin, B., & KEELINGC,. D. 1963. Large scale at- Quart. J . Royal MeteoT. SOC.,7 5 , 351-363. rnospheric mixing as deduced from the seasonal Danielsen, E. F. 1968. Stratospheric-tropospheric and meridional variations of carbon dioxide. J . exchange based on radioactivity, ozone and potenGeophys. Res., 68, 3899-3920. tial vorticity. J. Atmos. Sci., 25, 602-518.
    • Brewer, A. W. 1949. Evidence for a world circula- Junge, C. E. 1962a. Note on the exchange rate between the northern and southern atmosphere. Newell, R. E. 1963a. The general circulation of the Tellus, 14, 242-246. atmosphere and its effects on the movement of
    • Junge, C. E. 1962b. Global ozone budget and ex- trace substances. J. Weophya. Rea., 68, 3949-3962. change between stratosphere and troposphere. Newell, R. E. 1963b. Transfer through the tropoTellzca 14, 363-377. pause and within the stratosphere. Quart. J.
    • Junge, C. E. & Czeplak, G. 1968. Some aspects of Royal Meteor. SOC.,89, 167-204. the seasonal variation of carbon dioxide and Newell, R. E. 1964. Stratospheric energetics and ozone, Tellus 20, 422-434. mass transport. Pure and Applied Weophys., 58,
    • Kao, S.-K. 1962. Large-scale turbulent diffusion in a 145-156. rotating fluid with applications to the atmos- Newell, R. E. 8. Miller, A. J. 1965. Some aspects phere. J. Weophya. Res., 67, 2347-2359. of the general circulation of the lower stratos-
    • Kao, S.-K. & Bullock, W. S. 1964. Lagrangian and phere. Proceedings of the Second AEC Conference Eulerian correlations and energy spectra of geo- on radioactive fallout from nuclear weapons tests, strophic velocities. Quart. J. Royal Meteor. SOC., Nov. 3-6, 1964, United States Atomic Energy 90, 166-174. Commksion, Symposium series 5, 392-404.
    • Kao, S.-K. 1965. Some aspects of the large-scale Newell, R. E., Wallace, J. M. & Mahoney, J. R. 1966. turbulence and diffusion in the atmosphere. Quart. The general circulation of the atmosphere and its J. Royal Meteor. SOC.9,1, 10-17. effects on the movement of trace substances.
    • Kao, S.-K. & Al-Gain, A. A. 1968. Large-scale dis- Part 2, Tellua, 18, 363-380. persion of clusters of particles in the atmosqhere. Newell, R. E. & Miller, A. J. 1968. Vertical velocity J. Atmoa. Sci., 25, 214-221. variability in the lower stratosphere. J. Applied
    • Kennedy, J. S. 1964. Energy generation through Meteor., 7, 516-518. radiative processes in the lower stratosphere. Rodgers, C. D. 1967. The radiative heat budget of Rept. No. 11, Planetary Circulations Project, Dept. the troposphere and lower stratosphere. Rept. No. of Meteorology, M.I.T., Contract AT(30-1)2241. A2, Planetary Circulations Project, Dept. of
    • Kidson, J. W., Vincent, D. G. & Newell, R. E. 1969. Meteorology, M.I.T., Contract AT(30-1)2241. Observational studies of the general circulation Vincent, D. G. 1968. Mean meridional circulations of the tropics. I. Long term values. Quart. J. in the northern hemisphere lower stratosphere Royal Meteor. SOC.(in press). during 1964 and 1965. Quart. J. Royal Meteor.
    • Mastenbrook, H. J. 1968. Water vapor distribution SOC., 94, 333-349. in the stratosphere and high troposphere. J. Atmoa. sci., 25, 299-311.
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