期刊文献+

Experimental demonstration of the coupling effect of vertical velocity on latent heat flux

Experimental demonstration of the coupling effect of vertical velocity on latent heat flux
原文传递
导出
摘要 According to the cross coupling theorem of atmospheric turbulence, latent heat flux comprises two components, a vertical humidity gradient flux and a coupling flux of vertical velocity. In this paper, observational data are employed to demonstrate and analyze the coupling effect of vertical velocity on latent heat flux. The results highlight the presence of a coupling zero-effect height. When the observational level exceeds or underlies the coupling zero-effect height, the coupling effect suppresses or enhances the latent heat flux, respectively. Above the heterogeneous terrain in the experimental region, the overall difference between the estimated and the observed latent heat fluxes decreases from 27% to 2% (for ascending flow) and from 47% to 28% (for descending flow), after compensating for gradient flux. The coupling theorem of atmospheric turbulence is well validated by our analysis, supporting a role for experimental datasets in unraveling the mysteries of atmospheric turbulence. According to the cross coupling theorem of atmospheric turbulence, latent heat flux comprises two components, a vertical hu- midity gradient flux and a coupling flux of vertical velocity. In this paper, observational data are employed to demonstrate and analyze the coupling effect of vertical velocity on latent heat flux. The results highlight the presence of a coupling zero-effect height. When the observational level exceeds or underlies the coupling zero-effect height, the coupling effect suppresses or enhances the latent heat flux, respectively. Above the heterogeneous terrain in the experimental region, the overall difference between the estimated and the observed latent heat fluxes decreases from 27% to 2% (for ascending flow) and from 47% to 28% (for descending flow), after compensating for gradient flux. The coupling theorem of atmospheric turbulence is well val- idated by our analysis, supporting a role for experimental datasets in unraveling the mysteries of atmospheric turbulence.
出处 《Science China Earth Sciences》 SCIE EI CAS 2013年第4期684-692,共9页 中国科学(地球科学英文版)
基金 supported by National Natural Science Foundation of China(Grant Nos. 40705007, 1141130961 & 91025011) the Hundred-Talent Project of Chinese Academy of Sciences granted to Dr. YU.
关键词 atmospheric surface layer (ASL) turbulent transport latent heat flux vertical velocity CROSS-COUPLING 耦合效应 潜热通量 垂直速度 实验演示 大气湍流 湿度梯度 观测数据 交叉耦合
  • 相关文献

二级参考文献22

共引文献59

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部