Reply to a comment by R.J. Smalley and R.A. Antonia on 'The local isotropy hypothesis and the turbulent kinetic energy dissipation rate in the atmospheric surface layer' (October 13, 2004, 130, 2733-2752)

被引：0

作者：

Chamecki, M ^{[1
]}

Dias, NL ^{[1
]}

机构：

[1] Johns Hopkins Univ, Dept Geog & Environm Engn & Lemma, Lab Environm Monitoring & Modeling Anal, UFPR,IAPAR,SIMEPAR, BR-81531990 Curitiba, Parana, Brazil

来源：

QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY | 2006年 / 132卷 / 615期

关键词：

homogeneous turbulence; inertial subrange; velocity-velocity-increment correlation;

D O I：

10.1256/qj.05.144A

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

In response to Smalley and Antonia's comment, we agree that our statement that closer-to-zero velocity-velocity-increment correlation for larger turbulence intensity values cannot be taken as a measure of homogeneity. We also explain that, although not aware that the velocity-velocity-increment correlation cannot be zero at finite r1, we concentrated most of our analysis on its tendency towards zero with decreasing r1, since this limit is well known for homogeneous turbulence. © Royal Meteorological Society, 2006.

引用

页码：685 / 686

页数：2