摘要
本文首先对Deardorff的一阶模型给予解释 ,在此基础上根据对流边界层湍流动能方程 ,分析机械湍流和对流湍流对边界层发展的贡献 ,提出一个新的速度尺度———混合层顶速度尺度 ,定义了全理查森数 ,给出夹卷层厚度的参数化方案 ,并用Boers和Elotanta的雷达观测数据进行验证 .参数化方案与实验数据符合得很好 .当夹卷层厚度表示为夹卷速度或夹卷理查森数的函数时 ,该函数曲线随边界层发展表现为磁滞回线形状现象 ,文中对此进行了解释 .
An explanation about the first-order model of Deardorff is given. Based on this explain, the turbulent kinetic energy equation is analyzed, and the contribution to evolution of the convective boundary layer is divided into two parts: buoyant production and mechanical production. Thereout, a new velocity scale, top velocity scale of mixed layer, is proposed. At the same time, the full Richardson number is defined. And a new parameterization of thickness of entrainment zone is concluded. It gives a good agreement with the data of Boers and Eloranta measured by lidar. When the entrainment zone thickness normalized by mixed-layer depth is ploted as a function of the entrainment Richardson number or the entrainment rate normalized by the convective velocity scale, the curve of the function behaves as hysteresis. A preliminary interpretation is made to this phenomenon.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2005年第1期19-24,共6页
Chinese Journal of Geophysics
基金
国家自然科学基金(40105002
40333027)
中国科学院安徽光学精密机械研究所大气光学重点实验室科学基金(200201)共同资助
关键词
对流湍流
剪切湍流
混合层
夹卷层
参数化
Convective tubulence, Shear tubulence, Mixed layer, Entrainment zone, Parameterization.