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Mark R. Schoeberl and Marvin A. Geller

Auaus~r1977 MARK R. SCHOEBERL AND MARVIN A. GELLER 1235A Calculation of the Structure of Stationary Planetary Waves in Winter MARK R. SCHOEBERLt Aeronomy Laboratory, University of Illinois at Urbana-Champaign, Urbana 61801 MARW~ A. G~n~2A eronomy Laboratory and Laboratory for Atmospheric Research, Univ~sity of Illinois at Urbana-Champaign, Urbana 61801(Manuscript

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Y. Hayashi and D. G. Golder

VOL. 37, NO. 4 JOURNAL OF THE ATMOSPHERIC SCIENCES APRIL 1980The Seasonal Variation of Tropical Transient Planetary Waves Appearing in a GFDL General Circulation Model Y. HAYASHI AND D. G. GOLDERGeophysical Fiuid Dynamics Laboratory/NOAA, Princeton University, Princeton, NJ 08540(Manuscript received 28 February 1979, in final form 28 November 1979) ABSTRACT The seasonal variation of tropical transient

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Shyh-Chin Chen and Kevin E. Trenberth

15FEBRUARY 1988 SHYH-CHIN CHEN AND KEVIN E. TRENBERTH 657Orographically Forced Planetary Waves in the Northern Hemisphere Winter:Steady State Model with Wave-Coupled Lower Boundary Formulation SHYH-CHIN CHENDepartment of Atmospheric Sciences, University of lllinois, Urbana, Illinois KEVIN E. TRENBERTHNational Center for Atmospheric Research,* Boulder, Colorado(Manuscript received 25

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Hisannori Itoh

I MAY 1985 HISANORI ITOH 917The Role of Transient Motions in the Formation of Quasi-Stationary Planetary Waves HISANORI ITOHDepartment of Earth Sciences, Faculty of Education, Wakayama University, Wakayama, 640 Japan(Manuscript received 10 September 1984, in final form 22 Janumy 1985) ABSTRACT We investigate numerically, using bifurcation theory, the formation of quasi

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Taroh Matsuno

1970 T A R O H M A T S U N O 871Vertical Propagation of Stationary Planetary Waves in the Winter Northern Hemisphere TAROH MATSUNO~Deptr of Atmospheric Sciences, University of Washington, Seattle(Manuscript received 16 March 1970)ABSTRACT Planetary-scale, stationary disturbances in the winter stratosphere are considered to be upward propagating internal Rossby waves forced

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V. Hayashi and D. G. Golder

APRIL I983 Y. HAYASHI AND D. G. GOLDER 951Transient Planetary Waves Simulated by GFDL Spectral General Circulation Models. Part II: Effects of Nonlinear Energy Transfer Y. HAYASHI AND D. G. GOLDERGeophysical Fluid Dynamics Laboratory/NOlO`4, Princeton University, .Princeton, NJ 08540(Manuscript received 20 April 1982, in final form 12 November 1982) ABSTRACT

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Nili Harnik and Richard S. Lindzen

1. Introduction and motivation In this work we study how the basic-state wave propagation characteristics, and in particular the geometry of reflecting surfaces, affect the variability in the vertical structure of stratospheric planetary waves in a simple model and in observations of the Southern Hemisphere winter. The most common theory for stratospheric planetary waves is linear wave theory. Charney and Drazin (CD; 1961) were the first to treat stratospheric perturbations as vertically

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C.B. Leovy, C-R. Sun, M.H. Hitchman, E.E. Remsberg, J.M. Russell, III, L.L. Gordley, J.C. Gille, and L.V. Lyjak

230 JOURNAL OF THE ATMOSPHERIC SCIENCES VOL. 42, NO. 3Transport of Ozone in the Middle Stratosphere: Evidence for Planetary Wave BreakingC. B. L-ovY, C-R. SUN, M. H. HITCHMAN AND E. E. REMSBERG1Department of Atmospheric Sciences, University of Washington, Seattle, W/I 98195 J. M. RUSSELL, III AND L. L. G-ORDLEYNASA Langley Research Center, Hampton. VA 23665 J. C. GILLE AND L. V. LYJAKNational Center for Atmospheric Research

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John P. Boyd

756 JOURNAL OF THE ATMOSPHERIC SCIENCES VOLUME39The Influence of Meridionai Shear on Planetary Waves. Part 1: Nonsingular Wind Profiles JOHN P. BOYDICenter for Earth and Planetary Physics, Harvard University, Cambridge. M,4 02138(Manuscript received 9 March 1981, in final form 3 December 1981 ) ABSTRACT Using a simple separable model in which the mean wind U(y) is

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Ioana M. Dima and John M. Wallace

1. Introduction The equatorial planetary waves (EPW), forced by zonal asymmetries in the distribution of diabatic heating, are an important element in the global general circulation. They force the zonal flow by inducing equatorward eddy fluxes of westerly momentum at the jet stream level. In the annual mean, the eddy flux convergence would produce a strong equatorial superrotation were it not balanced by a flux divergence of westerly momentum by the zonally symmetric component of the

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