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    Vorticity, Momentum and Divergence Budgets of Synoptic-Scale Wave Disturbances in the Tropical Eastern Atlantic 

    Source: Monthly Weather Review:;1979:;volume( 107 ):;issue: 005:;page 535
    Author(s): Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: The budgets of vorticity, momentum and divergence are evaluated for the average synoptic-scale wave composited by Thompson et al. (1979) from Phase III data of the GARP Atlantic Tropical Experiment (GATE). The data are ...
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    On Symmetric Stability and Instability of Zonal Mean Flows Near the Equator 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 004:;page 882
    Author(s): Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: Obserations of longitudinally-averaged zonal flows in the atmosphere and ocean tend to display north?south symmetry about the equator, with a characteristic wind maximum or minimum, and therefore little horizontal wind ...
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    The Effect of Horizontal Pressure Gradients on the Momentum Transport in Tropical Convective Lines. Part II: Lagrangian Calculations 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 015:;page 2088
    Author(s): Flatau, Maria; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: The movement of a set of Lagrangian parcels in the two-dimensional pressure field associated with a tropical convective line is considered. The results are compared with observational characteristics of GATE quasi-two-dimensional ...
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    The Effect of Horizontal Pressure Gradients on the Momentum Transport in Tropical Convective Lines. Part I: The Results of the Convective Parameterization 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 015:;page 2074
    Author(s): Flatau, Maria; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: Measuremenits of the momentum transport in tropical convective lines suggest that horizontal momentum can be generated by the pressure low located near the center of the convective part of the line. A simple convective ...
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    The Role of Outflow-Layer Instabilities in Tropical Cyclone Motion 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 012:;page 1721
    Author(s): Flatau, Maria; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: The paper examines the role of the development of outflow-layer instabilities on the motion of tropical cyclones. The influence of barotropic instability is examined by comparing the time changes in the storm tracks with ...
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    Barotropic Instability with Downstream and Asymmetric Cross-Stream Variations: Idealized Calculations 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 001:;page 5
    Author(s): Crum, Francis X.; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: The barotropic instability of basic states with downstream and asymmetric cross-stream variations is investigated using the linearized, non-divergent barotropic vorticity equation in a periodic beta channel. A single ...
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    The Response of the Tropical Atmosphere to Low Frequency Thermal Forcing 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 004:;page 676
    Author(s): Anderson, John R.; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: The tropical response to a localized thermal forcing with approximately 45-day period is investigated for several models of increasing complexity consisting of two equivalent shallow water system and two fully stratified ...
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    The Presence of Linear Wavelike Modes in a Zonally Symmetric Model of the Tropical Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 015:;page 2115
    Author(s): Anderson, John R.; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: The linear, zonally symmetric modes of the basic state of a Hadley cell are examined. We find that the inclusion of the divergent basic state leads to the formation of a new class of slowly oscillating modes, some of which ...
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    Long Atmospheric Waves and the Polar-Plane Approximation to the Earth’s Spherical Geometry 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 003:;page 534
    Author(s): Bridger, Alison F. C.; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: The spherical geometry of the earth is replaced by polar cylindrical geometry, with a plane tangential to the earth at the pole. The resulting frequency and structure of free motions in an isothermal, adiabatic atmosphere ...
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    Numerical Modeling of the Stratospheric Sudden Warming: Some Sensitivity Studies 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 003:;page 666
    Author(s): Bridger, Alison F. C.; Stevens, Duane E.
    Publisher: American Meteorological Society
    Abstract: A version of Holton's numerical model of the stratospheric sudden warming is found to be very sensitive to the assumed initial mean zonal wind distribution. In tests with three initial wind profiles, in only one case can ...
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