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    Combined Dynamics of Boundary and Interior Perturbations in the Eady Setting 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 013:;page 1549
    Author(s): Dirren, Sébastien; Davies, Huw C.
    Publisher: American Meteorological Society
    Abstract: A theoretical study is undertaken of the relative influence of intermediate-level, near-surface, and tropopause-level perturbations upon flow development and cyclogenesis. The study is based upon two complementary ...
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    Forced Waves on a Zonally Aligned Jet Stream 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 001:;page 73
    Author(s): Schwierz, Cornelia; Dirren, Sébastien; Davies, Huw C.
    Publisher: American Meteorological Society
    Abstract: The potential vorticity (PV) pattern in the vicinity of the jet stream takes the form of a narrow tube of enhanced PV gradient on the in situ isentropic surfaces. It is asserted that this distinctive structure can serve ...
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    A Data Assimilation Case Study Using a Limited-Area Ensemble Kalman Filter 

    Source: Monthly Weather Review:;2007:;volume( 135 ):;issue: 004:;page 1455
    Author(s): Dirren, Sébastien; Torn, Ryan D.; Hakim, Gregory J.
    Publisher: American Meteorological Society
    Abstract: Ensemble Kalman filter (EnKF) data assimilation experiments are conducted on a limited-area domain over the Pacific Northwest region of the United States, using the Weather Research and Forecasting model. Idealized surface ...
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    Seasonal Runoff Forecasting Using Precipitation from Meteorological Data Assimilation Systems 

    Source: Journal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 005:;page 959
    Author(s): Schär, Christoph; Vasilina, Lyudmila; Pertziger, Felix; Dirren, Sébastien
    Publisher: American Meteorological Society
    Abstract: In semiarid mountainous regions such as central Asia, runoff from snowmelt often represents the dominant contribution to river flow and freshwater supply during the dry season. The estimation of snow accumulation during ...
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