Intermittent Turbulence Associated with a Density Current Passage in the Stable Boundary Layer
Intermittent Turbulence Associated with a Density Current Passage in the Stable Boundary Layer
复制标题
DOI:
10.1023/a:1019969131774
复制
发表时间:
2002-11
影响因子:
4.3
通讯作者:
Jielun Sun;S. Burns;D. Lenschow;R. Banta;R. Newsom;R. Coulter;S. Frasier;T. Ince;C. Nappo;J. Cuxart;W. Blumen;X. Lee;Xinzhang Hu
中科院分区:
文献类型:
--
作者:
Jielun Sun;S. Burns;D. Lenschow;R. Banta;R. Newsom;R. Coulter;S. Frasier;T. Ince;C. Nappo;J. Cuxart;W. Blumen;X. Lee;Xinzhang Hu
Using the unprecedented observational capabilities deployed duringthe Cooperative Atmosphere-Surface Exchange Study-99 (CASES-99),we found three distinct turbulence events on the night of 18October 1999, each of which was associated with differentphenomena: a density current, solitary waves, and downwardpropagating waves from a low-level jet. In this study, we focus onthe first event, the density current and its associatedintermittent turbulence. As the cold density current propagatedthrough the CASES-99 site, eddy motions in the upper part of thedensity current led to periodic overturning of the stratifiedflow, local thermal instability and a downward diffusion ofturbulent mixing. Propagation of the density current induced asecondary circulation. The descending motion following the head ofthe density current resulted in strong stratification, a sharpreduction in the turbulence, and a sudden increase in the windspeed. As the wind surge propagated toward the surface, shearinstability generated upward diffusion of turbulent mixing. Wedemonstrate in detail that the height and sequence of the localthermal and shear instabilities associated with the dynamics ofthe density current are responsible for the apparent intermittentturbulence.