1) entrainment zone
夹卷层
1.
Entrainment zone(EZ) at the top of convective boundary layer is a transition layer between the atmospheric convective boundary layer(ACBL) and free atmosphere,the turbulence structure of entrainment zone is one of the main properties.
对流边界层顶部夹卷层是边界层和自由大气之间的过渡带,夹卷层的湍流结构是其主要特征之一。
2.
The results show that temperature structure in the entrainment zone differs from the structure of isotropic turbulence and contains a lots of large-scale coherent eddies.
利用室内水槽模拟大气对流边界层,并用多探头测量和光学方法测量分析夹卷层的夹卷过程和温度场结构。
2) entrainment zone depth
夹卷层厚度
1.
On the definition and parameterization of the entrainment zone depth at the top of convective boundary layer;
夹卷层厚度定义对其参数化的影响
2.
Parameterization for entrainment zone depth at the top of convective boundary layer;
对流边界层顶部夹卷层厚度特征及其参数化分析
3) mixed layer and entrainment zone
混合层和夹卷层
4) entrainment
[in'treinmənt]
夹卷
1.
The bias is common to the current OGCMs,which has been ascribed to the model deficiencies in the parameterization of entrainment and vertical mixing process.
这表明在赤道东太平洋及南美沿岸,温跃层的变化通过夹卷过程及垂直扩散过程可以显著影响混合层的温度,OGCM对这些过程描述不足是导致SST年际变化模拟偏弱的一个重要原因,通过强调这些过程可以改善模拟效果。
2.
A turbulent kinetic energy budget is used to parameterize the wind stress-induced vertical mixing (entrainment),in which the effect of salt on stratification intensity is considered.
采用湍流动能收支参数化风应力产生的垂直混合（夹卷），其中考虑了盐度对层结强度的影响。
3.
A turbulent kintetic energy budget is used to parameterize the wind stress-induced vertical mixing(entrainment).
建立二层非线性原始方程海洋模式，采用湍流动能收支参数化风应力产生的垂直混合（夹卷），研究海洋对不同强度和最大风速半径的静止热带气旋（ＴＣ）的响应。
5) entrainment rate
夹卷速度
1.
Based on the "first-order model" of convective boundary layer(CBL),an improved parameterization for the entrainment rate of CBL was proposed.
基于对流边界层“一阶模型”,并考虑机械湍流和夹卷过程对对流边界层发展的贡献,提出了对流边界层顶部夹卷速度参数化的改进方案。
2.
According to the data measured during CIRCE (Central Illinois Rainfall Chemistry Experiment), a comparison of two parameterization schemes about the entrainment rate at the top of the convective boundary layer has been made in this paper.
应用 1979年 7月美国CIRCE试验边界层观测资料对两个夹卷速度参数化方案进行了对比验证 ,结果表明 :基于简单夹卷层结构模型的参数化方案we/w =A·Ri- 1 只适用于自由对流边界层 ,当对流边界层中存在较强机械湍流时 ,该方案变得不再适用 ;而基于“侵吞模型”的参数化方案we/w =B·θ /(Γzi)则不仅适用于自由对流边界层 ,对于含有较强机械湍流的对流边界层也能较好地符合 ,因而具有较强的适用性 。
6) wind entrainment
风夹卷
补充资料：夹叙夹议
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