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    The Statistical Properties of a Zonal Jet in a Baroclinic Atmosphere: A Semilinear Approach. Part I: Quasi-geostrophic, Two-Layer Model Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 021:;page 3046
    Author(s): Speranza, A.; Malguzzi, P.
    Publisher: American Meteorological Society
    Abstract: A semilinear (the wave-dynamics are linear with the time-evolution operator determined by the time-varying zonal flow while the zonal flow is fully nonlinear in the eddy fluxes) model of a baroclinic zonal jet is integrated, ...
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    Statistical Properties of Low-Frequency Variability in the Northern Hemisphere 

    Source: Journal of Climate:;1989:;volume( 002 ):;issue: 004:;page 367
    Author(s): Benzi, R.; Speranza, A.
    Publisher: American Meteorological Society
    Abstract: We discuss some statistical properties of the observed tropospheric circulation in Northern Hemisphere mid-latitudes. The data used consist of the twice-daily 500 mb height NMC analyses for the period 1966?77. Our analysis ...
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    Local Multiple Equilibria and Regional Atmospheric Blocking 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 009:;page 1939
    Author(s): Malguzzi, P.; Speranza, A.
    Publisher: American Meteorological Society
    Abstract: Stationary flow of a barotropic fluid in a ? channel has been shown by Charney and De Vore (1979) to possess multiple-equilibrium solutions when sinusoidal topographic forcing is exerted within the region of resonance near ...
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    Orographic Instability of Nonsymmetric Baroclinic Flows and Nonpropagating Planetary Waves 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 023:;page 2585
    Author(s): Cessi, P.; Speranza, A.
    Publisher: American Meteorological Society
    Abstract: The theory of the baroclinic instability of a nonsymmetric basic state in the presence of shallow sinusoidal topography is analyzed. The limiting case of vanishing topography (instability of a baroclinic Rossby wave) is ...
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    A Theory of Deep Cyclogenesis in the Lee of the Alps. Part II: Effects of Finite Topographic Slope and Height 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 023:;page 2826
    Author(s): Buzzi, A.; Speranza, A.
    Publisher: American Meteorological Society
    Abstract: The theory of cyclogenesis in the lee of the Alps presented by Speranza et al. in Part I is reexamined here (Part II) in the context of models dealing with finite amplitude topography. This generalization leads to the ...
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    Effects of Finite Height Topography on Nongeostrophic Baroclinic Instability: Implications to Theories of Lee Cyclogenesis 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 011:;page 1475
    Author(s): Malguzzi, P.; Trevisan, A.; Speranza, A.
    Publisher: American Meteorological Society
    Abstract: Baroclinic instability in the presence of steep finite amplitude topography is studied in the primitive equation model. The quasi-geostrophic theory of Alpine cyclogenesis of Speranza et al. is reanalyzed and discussed in ...
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    Instabilities of a Baroclinic Flow Related to Topographic Forcing 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 004:;page 637
    Author(s): Buzzi, A.; Trevisan, A.; Speranza, A.
    Publisher: American Meteorological Society
    Abstract: The presence of bottom topography in a baroclinic flow modifies the properties of the propagating baroclinic unstable modes and allows for the appearance of new unstable modes which are nonpropagating, as first shown by ...
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    A Minimal Baroclinic Model for the Statistical Properties of Low-Frequency Variability 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 023:;page 2962
    Author(s): Benzi, R.; Speranza, A.; Sutera, A.
    Publisher: American Meteorological Society
    Abstract: A recent analysis of atmospheric observations has shown evidence of bimodality in the statistical distribution of wave amplitude in the ultralong (zonal wavenumber group 2?4), low frequency (period >5 days). Similar analysis ...
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    Nonlinear Amplification of Stationary Rossby Waves Near Resonance. Part I. 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 002:;page 298
    Author(s): Malguzzi, P.; Speranza, A.; Sutera, A.; Caballero, R.
    Publisher: American Meteorological Society
    Abstract: The authors search the stationary solutions of the barotropic vorticity equation in spherical coordinates by numerically solving the equations with the Newton?Keller pseudoarclength continuation method. The solutions consist ...
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    Nonlinear Amplification of Stationary Rossby Waves near Resonance. Part II 

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 020:;page 2441
    Author(s): Malguzzi, P.; Speranza, A.; Sutera, A.; Caballero, R.
    Publisher: American Meteorological Society
    Abstract: In a preceding paper the authors showed that planetary waves of very different amplitudes can be sustained on the same configuration of the zonal wind by asymptotically balancing the energy contributions related to Ekman ...
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