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    Large Eddy Simulation of Thermally Induced Oscillations in the Convective Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 018:;page 2328
    Author(s): Letzel, Marcus Oliver; Raasch, Siegfried
    Publisher: American Meteorological Society
    Abstract: Mesoscale circulations induced by differential boundary layer heating due to surface inhomogeneities on scales of 5 km and more can significantly change the average properties and the structure of the convective boundary ...
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    The Route to Raindrop Formation in a Shallow Cumulus Cloud Simulated by a Lagrangian Cloud Model 

    Source: Journal of the Atmospheric Sciences:;2017:;Volume( 074 ):;issue: 007:;page 2125
    Author(s): Hoffmann, Fabian; Noh, Yign; Raasch, Siegfried
    Publisher: American Meteorological Society
    Abstract: he mechanism of raindrop formation in a shallow cumulus cloud is investigated using a Lagrangian cloud model (LCM). The analysis is focused on how and under which conditions a cloud droplet grows to a raindrop by tracking ...
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    The Role of Preconditioning in the Evolution of Open-Ocean Deep Convection 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 006:;page 1145
    Author(s): Noh, Yign; Cheon, Woo Geun; Raasch, Siegfried
    Publisher: American Meteorological Society
    Abstract: Large-eddy simulation of open-ocean deep convection shows that the evolution of convection appears in a fundamentally different pattern, depending on the precondition of the ocean and the magnitude of the surface buoyancy ...
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    Large Eddy Simulation of the Ocean Mixed Layer: The Effects of Wave Breaking and Langmuir Circulation 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 004:;page 720
    Author(s): Noh, Yign; Min, Hong Sik; Raasch, Siegfried
    Publisher: American Meteorological Society
    Abstract: Large eddy simulation (LES) of the ocean mixed layer was performed in which both wave breaking and Langmuir circulation are realized. Wave breaking was represented by random forcing consistent with the observed near-surface ...
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    Examination of the Mixed Layer Deepening Process during Convection Using LES 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 009:;page 2189
    Author(s): Noh, Yign; Goh, Gahyun; Raasch, Siegfried
    Publisher: American Meteorological Society
    Abstract: Analysis of large-eddy simulation data of the ocean mixed layer under convection reveals that the contribution from wind stress decreases with time as a result of inertial oscillation in the extratropical ocean and that ...
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    Influence of Langmuir Circulation on the Deepening of the Wind-Mixed Layer 

    Source: Journal of Physical Oceanography:;2010:;Volume( 041 ):;issue: 003:;page 472
    Author(s): Noh, Yign; Goh, Gahyun; Raasch, Siegfried
    Publisher: American Meteorological Society
    Abstract: Analysis of large eddy simulation data reveals that Langmuir circulation (LC) induces a significant enhancement of the mixed layer deepening, only if the mixed layer depth (MLD) h is shallow and the buoyancy jump across ...
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    Formation of a Diurnal Thermocline in the Ocean Mixed Layer Simulated by LES 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 005:;page 1244
    Author(s): Noh, Yign; Goh, Gahyun; Raasch, Siegfried; Gryschka, Micha
    Publisher: American Meteorological Society
    Abstract: The formation of a diurnal thermocline in the ocean mixed layer under a stabilizing buoyancy flux was simulated successfully by large-eddy simulation, reproducing various features consistent with observation. The analysis ...
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    A Refinement of the Millionshchikov Quasi-Normality Hypothesis for Convective Boundary Layer Turbulence 

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 007:;page 2632
    Author(s): Gryanik, Vladimir M.; Hartmann, Jörg; Raasch, Siegfried; Schröter, Michael
    Publisher: American Meteorological Society
    Abstract: The Millionshchikov hypothesis of quasi-normal distribution of fourth-order moments fails for convective conditions where the probability density functions of temperature and vertical velocity fluctuations are skewed. This ...
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    A Large-Eddy Simulation Study of Thermal Effects on Turbulent Flow and Dispersion in and above a Street Canyon 

    Source: Journal of Applied Meteorology and Climatology:;2012:;volume( 051 ):;issue: 005:;page 829
    Author(s): Park, Seung-Bu; Baik, Jong-Jin; Raasch, Siegfried; Letzel, Marcus Oliver
    Publisher: American Meteorological Society
    Abstract: hermal effects on turbulent flow and dispersion in and above an idealized street canyon with a street aspect ratio of 1 are numerically investigated using the parallelized large-eddy simulation model (?PALM?). Each of ...
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