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    Dynamics of the Transient Negative Eddy Response to Zonal-Mean Zonal Wind Variations 

    Source: Journal of the Atmospheric Sciences:;2023:;volume( 080 ):;issue: 002
    Author(s): Lorenz, David J.
    Publisher: American Meteorological Society
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    A Simple Mechanistic Model of Wave–Mean Flow Feedbacks, Poleward Jet Shifts, and the Annular Mode 

    Source: Journal of the Atmospheric Sciences:;2023:;volume( 080 ):;issue: 002:;page 549
    Author(s): Lorenz, David J.
    Publisher: American Meteorological Society
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    Dynamics of the Transient Negative Eddy Response to Zonal-Mean Zonal Wind Variations 

    Source: Journal of the Atmospheric Sciences:;2023:;volume( 080 ):;issue: 002:;page 593
    Author(s): Lorenz, David J.
    Publisher: American Meteorological Society
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    Understanding Midlatitude Jet Variability and Change Using Rossby Wave Chromatography: Methodology 

    Source: Journal of the Atmospheric Sciences:;2014:;Volume( 072 ):;issue: 001:;page 369
    Author(s): Lorenz, David J.
    Publisher: American Meteorological Society
    Abstract: ossby wave chromatography (RWC) is implemented in a linearized barotropic model as a tool to diagnose and understand the interaction between the midlatitude jet and the eddies. Given the background zonal-mean flow and the ...
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    Understanding Midlatitude Jet Variability and Change Using Rossby Wave Chromatography: Poleward-Shifted Jets in Response to External Forcing 

    Source: Journal of the Atmospheric Sciences:;2014:;Volume( 071 ):;issue: 007:;page 2370
    Author(s): Lorenz, David J.
    Publisher: American Meteorological Society
    Abstract: ossby wave chromatography (RWC) is implemented in a linearized barotropic model as a tool to understand the response of the midlatitude jet to external forcing. Given the background zonal-mean flow and the space?time ...
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    Understanding Midlatitude Jet Variability and Change Using Rossby Wave Chromatography: Wave–Mean Flow Interaction 

    Source: Journal of the Atmospheric Sciences:;2014:;Volume( 071 ):;issue: 010:;page 3684
    Author(s): Lorenz, David J.
    Publisher: American Meteorological Society
    Abstract: ossby wave chromatography (RWC) is implemented in a linearized barotropic model as a tool to understand the interaction between the midlatitude jet and the eddy momentum fluxes (u?) in an idealized GCM. Given the background ...
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    A Simple Mechanistic Model of Wave–Mean Flow Feedbacks, Poleward Jet Shifts, and the Annular Mode 

    Source: Journal of the Atmospheric Sciences:;2023:;volume( 080 ):;issue: 002
    Author(s): Lorenz, David J.
    Publisher: American Meteorological Society
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    Eddy–Zonal Flow Feedback in the Southern Hemisphere 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 021:;page 3312
    Author(s): Lorenz, David J.; Hartmann, Dennis L.
    Publisher: American Meteorological Society
    Abstract: The variability of the zonal-mean zonal wind in the Southern Hemisphere is studied using EOF analysis and momentum budget diagnostics of NCEP reanalysis data (1978?97). The leading EOF of the zonal-mean zonal wind is well ...
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    Eddy–Zonal Flow Feedback in the Northern Hemisphere Winter 

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 008:;page 1212
    Author(s): Lorenz, David J.; Hartmann, Dennis L.
    Publisher: American Meteorological Society
    Abstract: The variability of the zonal-mean zonal wind in the Northern Hemisphere winter (December?March) is studied using EOF analysis and momentum budget diagnostics of NCEP?NCAR reanalysis data (1976?2001). The leading EOF of the ...
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    The Signature of the Annular Modes in the Tropical Troposphere 

    Source: Journal of Climate:;2004:;volume( 017 ):;issue: 022:;page 4330
    Author(s): Thompson, David W. J.; Lorenz, David J.
    Publisher: American Meteorological Society
    Abstract: The extratropical annular modes are coupled with a distinct pattern of climate anomalies that spans the circulation of the tropical troposphere. The signature of the annular modes in the tropical troposphere exhibits a ...
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