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    Optimal Relationship of Large-Scale Flow Patterns and the Barotropic Feedback Due to High-Frequency Eddies 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 009:;page 1141
    Author(s): Metz, Werner
    Publisher: American Meteorological Society
    Abstract: A canonical correlation analysis is used to study the optimal relationship between low-frequency variations of the 500 mb height and the barotropic feedback effect in terms of cyclone-scale eddy-induced height tendencies. ...
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    Wintertime Blocking and Mountain Forcing of the Zonally-Averaged Flow: A Cross-Spectral Time Series Analysis of Observed Data 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 018:;page 1880
    Author(s): Metz, Werner
    Publisher: American Meteorological Society
    Abstract: Nine winters of Northern Hemisphere observations are used for a statistical analysis of the relation between the mountain forcing of the zonally-averaged barotropic wind and blocking. Thereby, the temporal variability of ...
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    Singular Modes and Low-Frequency Atmospheric Variability 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 012:;page 1740
    Author(s): Metz, Werner
    Publisher: American Meteorological Society
    Abstract: Recently, it has been shown that the EOFs (empirical orthogonal functions) of the solutions of a stationary linear model to an ensemble of white noise forcing fields are the Schmidt modes (singular modes) of the model' ...
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    Transient Eddy Forcing of Low-Frequency Atmospheric Variability 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 017:;page 2407
    Author(s): Metz, Werner
    Publisher: American Meteorological Society
    Abstract: This paper is concerned with the forcing of the low-frequency variability (10 days up to 3 months) of the barotropic planetary waves (wavenumbers 1 to 4) for wintertime conditions in the Northern Hemisphere. In particular, ...
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    Transient Cyclone-Scale Vorticity Forcing of Blocking Highs 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 014:;page 1467
    Author(s): Metz, Werner
    Publisher: American Meteorological Society
    Abstract: The forcing of Northern Hemisphere blocking highs by the transient vorticity transfer from the cyclone-scale eddies into the planetary flow is investigated. Thereby, a barotropic prediction model for the planetary modes ...
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    Low-Frequency Anomalies of Atmospheric Flow and the Effects of Cyclone-Scale Eddies: A Canonical Correlation Analysis 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 007:;page 1026
    Author(s): Metz, Werner
    Publisher: American Meteorological Society
    Abstract: Canonical correlation analysis is applied to investigate the relationship between the low-pass filtered (barotropic) streamfunction and the effects of cyclone-scale eddies. The eddy effects are evaluated in terms of flux ...
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    Transient-Eddy Feedbacks Derived from Linear Theory and Observations 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 023:;page 2743
    Author(s): Robertson, Andrew W.; Metz, Werner
    Publisher: American Meteorological Society
    Abstract: Linear baroclinic instability theory is used to investigate the subweekly time scale transient eddies (TEs) and their feedbacks associated with three-dimensional basic flows on the Northern Hemisphere, in terms of a two-layer ...
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    Three-Dimensional Linear Instability of Persistent Anomalous Large-Scale Flows 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 018:;page 2783
    Author(s): Robertson, Andrew W.; Metz, Werner
    Publisher: American Meteorological Society
    Abstract: The linear baroclinic instability of three-dimensional basic flows on the Northern Hemisphere is examined in terms of a simple two-level, quasi-geostrophic model. The basic flows considered comprise an observed six-winter ...
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