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    Alpine Lee Cyclogenesis: Verification of Theories 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 015:;page 2187
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: A novel technique is used to test theories of Alpine lee cyclogenesis. An ?idealized? reference simulation of a cyclogenetic event is performed with a channel flow model. Recent theories of Speranza et al., Pierrehumbert, ...
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    Forced Rossby Waves in Observed Background Flows 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 015:;page 2176
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: We consider forced quasi-stationary Rossby waves in background flows with realistic variability in time and space. Long-term integrations of the nonlinear barotropic vorticity equation for deviations from background flow ...
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    Tropopause Height in Baroclinic Channel Flow 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 012:;page 2232
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: A wave?mean flow model of dry channel flow is used to investigate the processes that determine the height HT and the slope of the extratropical tropopause. Without baroclinic waves, differential radiative heating and a ...
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    The Linear Response of a Hemispheric Two–Level Primitive Equation Model to Forcing by Topography 

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 004:;page 351
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: A hemispheric solution is obtained for the topographically forced stationary linear perturbations in a two-layer primitive equation model of the atmosphere. Results are discussed for January conditions. Additionally, the ...
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    Stochastically Driven Large-scale Circulations with Multiple Equilibria 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 012:;page 2606
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: The dynamic climatology of a simple model of barotropic stochastically forced ?-plane flow over topography is studied. Except for the forcing, the model is similar to the three-component systems studied by Charney and ...
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    Slope Winds and the Axisymmetric Circulation over Antarctica 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 017:;page 1859
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: An axisymmetric model of the flow over Antarctica is used to study the circulation induced by cooling of the air at the slopes of the continent. It is found that the resulting circulation with southeasterly surface winds ...
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    Valley Winds and the Diurnal Circulation over Plateaus 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 010:;page 2177
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: The role of valley winds in the diurnal circulation of large-scale mountain massifs like the Tibetan Plateau is investigated. We consider a circular plateau with radial valleys leading to the surrounding lowlands. A ...
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    On the Linear Theory of the Atmospheric Response to Sea Surface Temperature Anomalies 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 004:;page 603
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: A linear, hemispheric, two-level model which is based on the primitive equations is used to study the steady-state response of the atmosphere to sea surface temperature anomalies (SSTA's). First it is shown by comparison ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 009:;page 1824
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Dynamics of Blocking Highs 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 010:;page 1788
    Author(s): Egger, J.
    Publisher: American Meteorological Society
    Abstract: It is proposed that the nonlinear interaction of forced waves and slowly moving free waves May lead to the development of blocking highs under favorable conditions. This idea is tested numerically for three types of ...
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