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    The Formation of Wider and Deeper Clouds as a Result of Cold-Pool Dynamics 

    Source: Journal of the Atmospheric Sciences:;2014:;Volume( 071 ):;issue: 008:;page 2842
    Author(s): Schlemmer, Linda; Hohenegger, Cathy
    Publisher: American Meteorological Society
    Abstract: his study investigates how precipitation-driven cold pools aid the formation of wider clouds that are essential for a transition from shallow to deep convection. In connection with a temperature depression and a depletion ...
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    Mountain Volume Control on Deep-Convective Rain Amount during Episodes of Weak Synoptic Forcing 

    Source: Journal of the Atmospheric Sciences:;2019:;volume 076:;issue 002:;page 605
    Author(s): Imamovic, Adel; Schlemmer, Linda; Schär, Christoph
    Publisher: American Meteorological Society
    Abstract: Thermally driven upslope flows in mountainous areas provide favorable conditions for diurnal deep moist convection especially during episodes of weak synoptic forcing. The present study investigates the response of deep ...
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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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    Influence of the Background Wind on the Local Soil Moisture–Precipitation Feedback 

    Source: Journal of the Atmospheric Sciences:;2013:;Volume( 071 ):;issue: 002:;page 782
    Author(s): Froidevaux, Paul; Schlemmer, Linda; Schmidli, Juerg; Langhans, Wolfgang; Schär, Christoph
    Publisher: American Meteorological Society
    Abstract: he importance of soil moisture anomalies on airmass convection over semiarid regions has been recognized in several studies. The underlying mechanisms remain partly unclear. An open question is why wetter soils can result ...
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    Disentangling the Forcing Mechanisms of a Heavy Precipitation Event along the Alpine South Side Using Potential Vorticity Inversion 

    Source: Monthly Weather Review:;2009:;volume( 138 ):;issue: 006:;page 2336
    Author(s): Schlemmer, Linda; Martius, Olivia; Sprenger, Michael; Schwierz, Cornelia; Twitchett, Arwen
    Publisher: American Meteorological Society
    Abstract: Extreme precipitation events along the Alpine south side (AS) are often forced by upper-level positive potential vorticity (PV) anomalies over western Europe. These so-called PV streamers go along with a dynamical forcing ...
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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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    Validation of a High-Resolution Numerical Weather Prediction Land Surface Scheme Using Catchment Water Balances 

    Source: Journal of Hydrometeorology:;2021:;volume( 022 ):;issue: 012:;page 3189
    Author(s): Regenass, Daniel;Schlemmer, Linda;Fuhrer, Oliver;Bettems, Jean-Marie;Arpagaus, Marco;Schär, Christoph
    Publisher: American Meteorological Society
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