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    Turbulent Mixing within Tropopause Folds as a Mechanism for the Exchange of Chemical Constituents between the Stratosphere and Troposphere 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 005:;page 994
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: Evidence is presented which illustrates the role of jet stream-frontal zone clear air turbulence (CAT) as a mechanism for the exchange of air and chemical trace constituents between the stratosphere and the troposphere. ...
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    The Role of Turbulent Heat Flux in the Generation of Potential Vorticity in the Vicinity of Upper-Level Jet Stream Systems 

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 007:;page 892
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: Results from three case study investigations of upper-level jet stream systems document the existence of stratospheric mesoscale cyclonic wind shear in the layer of maximum wind. Anomalously high values of potential vorticity ...
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    Frontogenesis and Geostrophically Forced Secondary Circulations in the Vicinity of Jet Stream-Frontal Zone Systems 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 005:;page 954
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: Frontogenesis and geostrophically forced secondary circulations in the vicinity of jet stream-frontal zone systems are treated, assuming that the motions conform to the geostrophic momentum approximation and that the ...
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    Meteorological Tower Measurements of a Surface Cold Front 

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 008:;page 1634
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: measurements from the Boulder Atmospheric Observatory meteorological research tower are used to describe the structure and physical processes of a strong surface cold front. Analysis reveals that the horizontal gradients ...
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    Dropwindsonde Observations of an Icelandic Low and a Greenland Mountain-Lee Wave 

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 004:;page 680
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Further Evidence of the Mesoscale and Turbulent Structure of Upper Level Jet Stream–Frontal Zone Systems 

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 008:;page 1100
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: Recent aircraft observations of the mesoscale and turbulent structure of upper level frontal zone-jet stream systems provide further evidence of stratosperic mesoscale cyclonic wind shear and associated anomalously high ...
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    A Multiple Structured Frontal Zone-Jet Stream System as Revealed by Meteorologically Instrumented Aircraft 

    Source: Monthly Weather Review:;1974:;volume( 102 ):;issue: 003:;page 244
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: The distribution of wind, temperature, ozone, and turbulence within a multiple structured frontal zone-jet stream system is described using a combination of direct horizontal measurements by meteorologically-instrumented ...
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    Simulation of Upper-Level Frontogenesis with a 20-Level Isentropic Coordinate Primitive Equation Model 

    Source: Monthly Weather Review:;1975:;volume( 103 ):;issue: 007:;page 591
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: A numerical simulation using the inviscid adiabatic primitive equations for atmospheric motion framed in isentropic coordinates is shown to generate upper-level frontogenesis with physical and dynamical similarity to that ...
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    On the Applicability of the Geostrophic Approximation to Upper-Level Frontal-Scale Motions 

    Source: Journal of the Atmospheric Sciences:;1970:;Volume( 027 ):;issue: 003:;page 408
    Author(s): Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: The techniques of scale-analysis and case-study diagnosis are used to establish a theory of meteorological approximations for upper-level frontal zones. A scale-analysis of the governing equations reveals that. 1) the ...
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    A Review of the Structure and Dynamics of Upper-Level Frontal Zones 

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 002:;page 452
    Author(s): Keyser, Daniel; Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: This article presents a review of upper-level fronts with the intent of synthesizing observational and modeling studies into a conceptual and dynamical description of these fronts and their evolution relative to the life ...
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