Results 21 to 30 of about 8,818 (209)
Lower‐tropospheric stability (LTS) and estimated inversion strength (EIS) have a widely accepted relationship with low cloud amount and are key observational foundations for understanding and modeling low‐level stratiform clouds.
Lauren Cutler +2 more
doaj +1 more source
Study of the Aerosol Indirect Effect by Large-Eddy Simulation of Marine Stratocumulus [PDF]
A total of 98 three-dimensional large-eddy simulations (LESs) of marine stratocumulus clouds covering both nighttime and daytime conditions were performed to explore the response of cloud optical depth (τ) to various aerosol number concentrations (Na ...
Lu, Miao-Ling, Seinfeld, John H.
core +1 more source
Scaling of Drizzle Virga Depth With Cloud Thickness for Marine Stratocumulus Clouds
Drizzle is frequently observed in marine stratocumulus clouds and plays a crucial role in cloud lifetime and the radiation budget. Most drizzling stratocumulus clouds form drizzle virga below cloud base, where subcloud scavenging and evaporative cooling ...
Fan Yang +4 more
doaj +1 more source
Influences of an entrainment–mixing parameterization on numerical simulations of cumulus and stratocumulus clouds [PDF]
Different entrainment–mixing processes can occur in clouds; however, a homogeneous mixing mechanism is often implicitly assumed in most commonly used microphysics schemes.
X. Xu +10 more
doaj +1 more source
Turbulent dispersion in cloud-topped boundary layers [PDF]
Compared to dry boundary layers, dispersion in cloud-topped boundary layers has received less attention. In this LES based numerical study we investigate the dispersion of a passive tracer in the form of Lagrangian particles for four kinds of atmospheric
Heus, T. +3 more
core +4 more sources
Factors Controlling Rapid Stratocumulus Cloud Thinning
Abstract The relationship between the inversion stability and the liquid water path (LWP) tendency of a vertically well-mixed, adiabatic stratocumulus cloud layer is investigated in this study through the analysis of the budget equation for the LWP.
J. J. van der Dussen +2 more
openaire +4 more sources
Multiple‐scale simulations of stratocumulus clouds [PDF]
This study introduces a flexible multiple nested modeling framework developed from the Weather Research and Forecasting (WRF) model for boundary layer cloud research. It features a nested large‐eddy simulation in a hindcasting mode that allows a direct comparison between simulations and observations.
Ping Zhu +3 more
openaire +1 more source
Impacts of solar-absorbing aerosol layers on the transition of stratocumulus to trade cumulus clouds [PDF]
The effects of an initially overlying layer of solar-absorbing aerosol on the transition of stratocumulus to trade cumulus clouds are examined using large-eddy simulations.
X. Zhou +5 more
doaj +1 more source
Phase 1 of the CGILS large‐eddy simulation (LES) intercomparison is extended to understand if subtropical marine boundary‐layer clouds respond to idealized climate perturbations consistently in six LES models.
Peter N. Blossey +6 more
doaj +1 more source
Simulation of marine stratocumulus using the super-droplet method: numerical convergence and comparison to a double-moment bulk scheme using SCALE-SDM 5.2.6-2.3.1 [PDF]
The super-droplet method (SDM) is a Lagrangian particle-based numerical scheme for cloud microphysics. In this work, a series of simulations based on the DYCOMS-II (RF02) setup with different horizontal and vertical resolutions are conducted to explore ...
C. Yin +4 more
doaj +1 more source

