The Convective Boundary Layer in the Terra Incognita

被引:113
作者
Zhou, Bowen [1 ,2 ,3 ]
Simon, Jason S. [4 ]
Chow, Fotini K. [4 ]
机构
[1] Nanjing Univ, MOE, Key Lab Mesoscale Severe Weather, Nanjing 210008, Jiangsu, Peoples R China
[2] Nanjing Univ, Sch Atmospher Sci, Nanjing 210008, Jiangsu, Peoples R China
[3] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Div Earth Sci, Berkeley, CA 94720 USA
[4] Univ Calif Berkeley, Dept Civil & Environm Engn, Berkeley, CA 94720 USA
基金
美国国家科学基金会;
关键词
NONHYDROSTATIC ATMOSPHERIC SIMULATION; PREDICTION SYSTEM ARPS; LARGE-EDDY-SIMULATION; VERTICAL DIFFUSION; MODEL; INSTABILITY; RESOLUTION; FLOW;
D O I
10.1175/JAS-D-13-0356.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Numerical simulations of a convective boundary layer (CBL) are performed to investigate model behavior in the terra incognita, also known as the gray zone. The terra incognita of the CBL refers to a range of model grid spacing that is comparable to the size of the most energetic convective eddies, which are on the order of the boundary layer depth. Using the Rayleigh-Benard thermal instability as reference, a set of idealized simulations is used to show that gray zone modeling is not only a numerical challenge, but also poses dynamical difficulties. When the grid spacing falls within the CBL gray zone, grid-dependent convection can occur. The size of the initial instability structures is set by the grid spacing rather than the natural state of the flow. This changes higher-order flow statistics and poses fundamental difficulties for gray zone modeling applications.
引用
收藏
页码:2545 / 2563
页数:19
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