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Large-Eddy Simulation of Marine Atmospheric Boundary Layers above a Spectrum of Moving Waves

机译：移动波谱上海洋大气边界层的大涡模拟

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Peter P. Sullivan; James C. Mcwilliams; Edward G. Patton;
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1. Large-Eddy Simulation of Marine Atmospheric Boundary Layers above a Spectrum of Moving Waves [J] . PETER P. SULLIVAN, JAMES C. MCWILLIAMS, EDWARD G. PATTON Journal of the Atmospheric Sciences . 2014,第11期

机译：运动波谱上方海洋大气边界层的大涡模拟
2. Large-eddy simulations and observations of atmospheric marine boundary layers above nonequilibrium surface waves [J] . Sullivan PP, Edson JB, Hristov T, Journal of the Atmospheric Sciences . 2008,第4期

机译：非平衡面波以上大气海洋边界层的大涡模拟与观测
3. Large-Eddy Simulations of Oil Droplet Aerosol Transport in the Marine Atmospheric Boundary Layer [J] . Meng Li, Ze Zhao, Yajat Pandya, Atmosphere . 2019,第8期

机译：海洋大气边界层中油滴气溶胶传输的大涡模拟
4. Entrainment and subgrid lengthscales in large-eddy simulations of atmospheric boundary-layer flows [C] . Bjorn Stevens, C. -H. Moeng, P. P. Sullivan IUTAM Symposium on Developments in Geophysical Turbulence . 2000

机译：大气边界层流动大涡模拟中的夹带和亚底纵数
5. Mixed-layer models and large-eddy simulations of stratocumulus-topped marine boundary layers: Their nonlinear dynamics and sensitivity to cloud droplet concentration. [D] . Uchida, Junya. 2010

机译：层积云顶海洋边界层的混合层模型和大涡模拟：它们的非线性动力学和对云滴浓度的敏感性。
6. The impact of cloud vertical profile on liquid water path retrieval based on the bispectral method: A theoretical study based on large-eddy simulations of shallow marine boundary layer clouds [O] . Daniel J. Miller, Zhibo Zhang, Andrew S. Ackerman, -1

机译：基于双谱法的云垂直剖面对液态水路径反演的影响：基于大涡模拟的浅海边界层云理论研究
7. Large-Eddy Simulations and Observations of Atmospheric Marine Boundary Layers above Nonequilibrium Surface Waves [O] . Peter P. Sullivan, James B. Edson, James C. Mcwilliams 2007

机译：非平衡面波上大气海洋边界层的大涡模拟与观测
8. Coordinated Parameterization Development and Large-Eddy Simulation for Marine and Arctic Cloud-Topped Boundary Layers [R] . Bretherton, Christopher S. 2002

机译：海洋和北极云顶边界层的协调参数化开发和大涡模拟

Large-Eddy Simulation of Marine Atmospheric Boundary Layers above a Spectrum of Moving Waves

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