HR: 1340h
AN: A53A-0909    [Abstracts]
TI: Turbulence Spectra in the Surface Layer with a Steady Surface Thermal Inversion
AU: Peng, Z
EM: pengzhen.iap@gmail.com
AF: Fei Hu, Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing 100029, People's Republic of China, Beijing, 100029,
AU: Hu, F
EM: hufei@mail.iap.ac.cn
AF: Fei Hu, Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing 100029, People's Republic of China, Beijing, 100029,
AU: Ma, X
EM: Maxg@mail.iap.ac.cn
AF: Xiaoguang Ma, Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing 100029, People's Republic of China, Beijing, 100029,
AU: * Liu, S
EM: lshuhua@pku.edu.cn
AF: Shuhua Liu, Group of Atmospheric Boundary Layer and Turbulence, Ministry Laboratory of Storm and Drought/Flood Damages,Department of Atmospheric Sciences, School of Physics, Peiking University, Beijing, China, Beijing, 100000,
AB: the EBEX-2000 (International Energy Balance Experiment, 2000, EBEX-2000) was carried out over a flood- irrigated cotton field with very strong evaporation and transpiration. And thus the latent heat flux took most part of the solar radiation and the sensible heat flux, which would directly heat the atmosphere, was very small and even became negative in mid-afternoon. Therefore, the thermal turbulence was suppressed and there always existed a surface thermal inversion during the observation. The temperatures measured at 8.7 m were always higher than that at 2.7 m, which further restrained the development of the turbulence in the lower part of the surface layer, and the turbulence exchanges for the momentum, energy and other were restrained too. Owing to strong action of the underlying surface, there is distinct wind shear, and the nearer the distance to the ground, the stronger the wind shear. Moreover, the surface thermal inversion makes the wind shear sustainable and stable. On the other hand, due to the strong blocking and friction action of the underlying surface, eddies would be strongly impacted when they came close to the ground, in particular for small eddies. That is to say, the nearer the distance to the ground, the stronger the influence of the ground on small eddies and the larger the range of eddy-size that can be directly influenced by the ground. Both the above factors contribute to the differences between the spectra at intermediate frequencies at the two heights: the horizontal power spectrum at 8.7 m does not obey -1 power law at intermediate frequencies, but it does at 2.7 m. The vertical power spectra at 8.7 m are somewhat flatter and broader at the spectral peak, while they are sharper and narrower at 2.7 m.
DE: 0312 Air/sea constituent fluxes (3339, 4504)
DE: 0315 Biosphere/atmosphere interactions (0426, 1610)
SC: Union [U]
MN: 2007 Fall Meeting