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    On Potential Vorticity Flux Vectors 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 023:;page 2917
    Author(s): Bannon, Peter R.; Schmidli, Jürg; Schär, Christoph
    Publisher: American Meteorological Society
    Abstract: Dynamical, rather than kinematical, considerations indicate that a generalized potential vorticity in terms of the gradient of an arbitrary scalar function requires that the potential vorticity flux vector contain a ...
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    Reconstruction of Mesoscale Precipitation Fields from Sparse Observations in Complex Terrain 

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 015:;page 3289
    Author(s): Schmidli, Jürg; Frei, Christoph; Schär, Christoph
    Publisher: American Meteorological Society
    Abstract: The feasibility of a statistical reconstruction of mesoscale precipitation fields over complex topography from a sparse rain gauge network is examined. Reconstructions of gridded monthly precipitation for the European Alps ...
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    Idealized Large-Eddy and Convection-Resolving Simulations of Moist Convection over Mountainous Terrain 

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 010:;page 4021
    Author(s): Panosetti, Davide; Böing, Steven; Schlemmer, Linda; Schmidli, Jürg
    Publisher: American Meteorological Society
    Abstract: n summertime fair-weather days, thermally driven wind systems play an important role in determining the initiation of convection and the occurrence of localized precipitation episodes over mountainous terrain. This study ...
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    An Idealized Cloud-Resolving Framework for the Study of Midlatitude Diurnal Convection over Land 

    Source: Journal of the Atmospheric Sciences:;2011:;Volume( 068 ):;issue: 005:;page 1041
    Author(s): Schlemmer, Linda; Hohenegger, Cathy; Schmidli, Jürg; Bretherton, Christopher S.; Schär, Christoph
    Publisher: American Meteorological Society
    Abstract: his paper introduces an idealized cloud-resolving modeling (CRM) framework for the study of midlatitude diurnal convection over land. The framework is used to study the feedbacks among soil, boundary layer, and diurnal ...
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