Effect of the entrainment flux ratio on the relationship between entrainment rate and convective richardson number

被引:25
作者
Jianning Sun [1 ,2 ]
Yuan Wang [1 ,2 ]
机构
[1] Nanjing Univ, Dept Atmospher Sci, Nanjing 210093, Jiangsu, Peoples R China
[2] Minist Educ, Key LAb Mesoscale Severe Weather, Nanjing 210093, Jiangsu, Peoples R China
关键词
convective Richardson number; entrainment rate; entrainment zone thickness; first-order jump model; total entrainment flux ratio;
D O I
10.1007/s10546-007-9231-4
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The parameterization of the dimensionless entrainment rate (w(e) /w(*)) versus the convective Richardson number (Ri(delta theta) ) is discussed in the framework of a first-order jump model (FOM). A theoretical estimation for the proportionality coefficient in this parameterization, namely, the total entrainment flux ratio, is derived. This states that the total entrainment flux ratio in FOM can be estimated as the ratio of the entrainment zone thickness to the mixed-layer depth, a relationship that is supported by earlier tank experiments, and suggesting that the total entrainment flux ratio should be treated as a variable. Analyses show that the variability of the total entrainment flux ratio is actually the effect of stratification in the free atmosphere on the entrainment process, which should be taken into account in the parameterization. Further examination of data from tank experiments and large-eddy simulations demonstrate that the different power laws for w(e) /w(*) versus Ri (delta theta) can be interpreted as the variability of the total entrainment flux ratio. These results indicate that the dimensionless entrainment rate depends not only on the convective Richardson number but also upon the total entrainment flux ratio.
引用
收藏
页码:237 / 247
页数:11
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