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    Transport, Moisture, and Rain in a Simple Monsoonlike Flow 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 011:;page 1817
    Author(s): Joseph, Binson; Moustaoui, Mohamed
    Publisher: American Meteorological Society
    Abstract: The Lagrangian transport of particles and its role in the redistribution of moisture and rainfall in a monsoonlike flow is investigated using a simple, dynamically consistent model of the heat-induced tropical circulation. ...
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    Relation between Kinematic Boundaries, Stirring, and Barriers for the Antarctic Polar Vortex 

    Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 007:;page 1198
    Author(s): Joseph, Binson; Legras, Bernard
    Publisher: American Meteorological Society
    Abstract: Maximum stretching lines in the lower stratosphere around the Antarctic polar vortex are diagnosed using a method based on finite-size Lyapunov exponents. By analogy with the mathematical results known for simple dynamical ...
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    Mixing Layer Formation near the Tropopause Due to Gravity Wave–Critical Level Interactions in a Cloud-Resolving Model 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 024:;page 3112
    Author(s): Moustaoui, Mohamed; Joseph, Binson; Teitelbaum, Hector
    Publisher: American Meteorological Society
    Abstract: A plausible mechanism for the formation of mixing layers in the lower stratosphere above regions of tropical convection is demonstrated numerically using high-resolution, two-dimensional (2D), anelastic, nonlinear, ...
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    Variability of Turbulence and Its Outer Scales in a Model Tropopause Jet 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 006:;page 621
    Author(s): Joseph, Binson; Mahalov, Alex; Nicolaenko, Basil; Tse, Kwan Leung
    Publisher: American Meteorological Society
    Abstract: Variability of flow regimes and turbulence scalings in a model of an inhomogeneously stratified, tropopause jet is investigated through high-resolution, forced, three-dimensional numerical simulations (with 512 or 1024 ...
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