Improved Length Scales for Turbulence Kinetic Energy-Based Planetary Boundary Layer Scheme for the Convective Atmospheric Boundary Layer

被引:8
|
作者
Zhou, Bowen [1 ,2 ]
Li, Yuhuan [3 ]
Zhu, Kefeng [1 ,2 ,4 ]
机构
[1] Nanjing Univ, Key Lab Mesoscale Severe Weather, Minist Educ, Nanjing, Peoples R China
[2] Nanjing Univ, Sch Atmospher Sci, Nanjing, Peoples R China
[3] China Meteorol Adm, Inst Urban Meteorol, Beijing, Peoples R China
[4] Chinese Acad Meteorol Sci, Nanjing Joint Inst Atmospher Sci, Nanjing, Peoples R China
基金
国家重点研发计划; 中国国家自然科学基金;
关键词
EDDY-DIFFUSIVITY; PART I; CLOSURE-MODEL; SURFACE-LAYER; PBL SCHEMES; PARAMETERIZATION; SIMULATION; DISSIPATION; ENTRAINMENT; SENSITIVITY;
D O I
10.1175/JAS-D-19-0334.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Based on a priori analysis of large-eddy simulations (LESs) of the convective atmospheric boundary layer, improved turbulent mixing and dissipation length scales are proposed for a turbulence kinetic energy (TKE)-based planetary boundary layer (PBL) scheme. The turbulent mixing length incorporates surface similarity and TKE constraints in the surface layer, and makes adjustments for lateral entrainment effects in the mixed layer. The dissipation length is constructed based on balanced TKE budgets accounting for shear, buoyancy, and turbulent mixing. A nongradient term is added to the TKE flux to correct for nonlocal turbulent mixing of TKE. The improved length scales are implemented into a PBL scheme, and are tested with idealized single-column convective boundary layer (CBL) cases. Results exhibit robust applicability across a broad CBL stability range, and are in good agreement with LES benchmark simulations. It is then implemented into a community atmospheric model and further evaluated with 3D real-case simulations. Results of the new scheme are of comparable quality to three other well-established PBL schemes. Comparisons between simulated and radiosonde-observed profiles show favorable performance of the new scheme on a clear day.
引用
收藏
页码:2605 / 2626
页数:22
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