Effects of Surface and Top Wind Shear on the Spatial Organization of Marine Stratocumulus‐Topped Boundary Layers
Author:
Affiliation:
1. Department of Mechanical and Aerospace Engineering University of California, San Diego La Jolla CA USA
2. Department of Physics Cleveland State University Cleveland OH USA
Funder
Comisión Nacional de Investigación Científica y Tecnológica
Biological and Environmental Research
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JD034162
Reference35 articles.
1. Mesoscale shallow convection in the atmosphere
2. Object‐Oriented Identification of Coherent Structures in Large Eddy Simulations: Importance of Downdrafts in Stratocumulus
3. A Joint Probability Density–Based Decomposition of Turbulence in the Atmospheric Boundary Layer
4. Daily variability of California coastal low cloudiness: A balancing act between stability and subsidence
5. Resolved Versus Parametrized Boundary-Layer Plumes. Part I: A Parametrization-Oriented Conditional Sampling in Large-Eddy Simulations
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1. Effects of Wind Shear and Aerosol Conditions on the Organization of Precipitating Marine Stratocumulus Clouds;Journal of Geophysical Research: Atmospheres;2023-12-18
2. Sensitivities of cloud radiative effects to large-scale meteorology and aerosols from global observations;Atmospheric Chemistry and Physics;2023-09-28
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