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    On the Role of Planetary-Scale Waves in the Abrupt Seasonal Transition of the Northern Hemisphere General Circulation 

    Source: Journal of the Atmospheric Sciences:;2013:;Volume( 071 ):;issue: 005:;page 1724
    Author(s): Shaw, Tiffany A.
    Publisher: American Meteorological Society
    Abstract: he role of planetary-scale waves in the abrupt seasonal transition of the Northern Hemisphere (NH) general circulation is studied. In reanalysis data, the winter-to-summer transition involves the growth of planetary-scale ...
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    Using the moist static energy budget to understand storm track shifts across a range of timescales 

    Source: Journal of the Atmospheric Sciences:;2017:;Volume( 074 ):;issue: 008:;page 2427
    Author(s): Barpanda, Pragallva; Shaw, Tiffany
    Publisher: American Meteorological Society
    Abstract: torm tracks shift meridionally in response to forcing across a range of timescales. Here we formulate a moist static energy (MSE) framework for storm track position and use it to understand storm track shifts in response ...
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    Connecting the Energy and Momentum Flux Response to Climate Change Using the Eliassen–Palm Relation 

    Source: Journal of Climate:;2018:;volume 031:;issue 018:;page 7401
    Author(s): Lachmy, Orli; Shaw, Tiffany
    Publisher: American Meteorological Society
    Abstract: AbstractCoupled climate models project that extratropical storm tracks and eddy-driven jets generally shift poleward in response to increased CO2 concentration. Here the connection between the storm-track and jet responses ...
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    The Impact of Stratospheric Model Configuration on Planetary-Scale Waves in Northern Hemisphere Winter 

    Source: Journal of Climate:;2010:;volume( 023 ):;issue: 012:;page 3369
    Author(s): Shaw, Tiffany A.; Perlwitz, Judith
    Publisher: American Meteorological Society
    Abstract: The impact of stratospheric model configuration on modeled planetary-scale waves in Northern Hemisphere winter is examined using the Canadian Middle Atmosphere Model (CMAM). The CMAM configurations include a high-lid (0.001 ...
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    On the Control of the Residual Circulation and Stratospheric Temperatures in the Arctic by Planetary Wave Coupling 

    Source: Journal of the Atmospheric Sciences:;2013:;Volume( 071 ):;issue: 001:;page 195
    Author(s): Shaw, Tiffany A.; Perlwitz, Judith
    Publisher: American Meteorological Society
    Abstract: t is well established that interannual variability of eddy (meridional) heat flux near the tropopause controls the variability of Arctic lower-stratospheric temperatures during spring via a modification of the strength of ...
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    The Life Cycle of Northern Hemisphere Downward Wave Coupling between the Stratosphere and Troposphere 

    Source: Journal of Climate:;2012:;volume( 026 ):;issue: 005:;page 1745
    Author(s): Shaw, Tiffany A.; Perlwitz, Judith
    Publisher: American Meteorological Society
    Abstract: he life cycle of Northern Hemisphere downward wave coupling between the stratosphere and troposphere via wave reflection is analyzed. Downward wave coupling events are defined by extreme negative values of a wave coupling ...
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    Tropical and Subtropical Meridional Latent Heat Transports by Disturbances to the Zonal Mean and Their Role in the General Circulation 

    Source: Journal of the Atmospheric Sciences:;2012:;Volume( 069 ):;issue: 006:;page 1872
    Author(s): Shaw, Tiffany A.; Pauluis, Olivier
    Publisher: American Meteorological Society
    Abstract: he spectrum of meridional latent heat transport in the tropics and subtropics by disturbances to the zonal mean during all seasons is analyzed. The transport is divided into stationary and transient planetary- and ...
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    Comments on “A Spectral Parameterization of Drag, Eddy Diffusion, and Wave Heating for a Three-Dimensional Flow Induced by Breaking Gravity Waves” 

    Source: Journal of the Atmospheric Sciences:;2011:;Volume( 068 ):;issue: 010:;page 2465
    Author(s): Shaw, Tiffany A.; Becker, Erich
    Publisher: American Meteorological Society
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    Dynamics of Extreme Stratospheric Negative Heat Flux Events in an Idealized Model 

    Source: Journal of the Atmospheric Sciences:;2018:;volume 075:;issue 010:;page 3521
    Author(s): Dunn-Sigouin, Etienne; Shaw, Tiffany
    Publisher: American Meteorological Society
    Abstract: AbstractRecent work has shown that extreme stratospheric wave-1 negative heat flux events couple with the troposphere via an anomalous wave-1 signal. Here, a dry dynamical core model is used to investigate the dynamical ...
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    Downward Wave Coupling between the Stratosphere and Troposphere: The Importance of Meridional Wave Guiding and Comparison with Zonal-Mean Coupling 

    Source: Journal of Climate:;2010:;volume( 023 ):;issue: 023:;page 6365
    Author(s): Shaw, Tiffany A.; Perlwitz, Judith; Harnik, Nili
    Publisher: American Meteorological Society
    Abstract: The nature of downward wave coupling between the stratosphere and troposphere in both hemispheres is analyzed using the 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) dataset. Downward ...
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