热带沿海近地层大气的湍流结构和谱特征
SPECTRAL AND TURBULENT CHARACTERISTICS IN THE NEAR SURFACE ATMOSPHERIC LAYER OVER TROPICAL COASTAL AREA
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摘要: 利用1990年在海南省海口市天尾村的一次观测的资料,分析了速度分量谱、湍流强度等湍流特征量。这批资料多是有云影响情况下,稳定度参数(L)与热通量(wt)没有日变化规律,但湍能、平均温度仍具有日变化规律;湍谱的基本特征与晴天天气的谱基本相似,在惯性副区接近局地各向同性,速度谱符合相似理论的“-2/3”次方规律;根据M-O相似理论,探讨了各分量湍强δi/U*(i=u,v,w)与稳定度Z/L的关系,表明各分量湍强与稳定度Z/L仍具有“1/3”次方规律,但湍强和湍流能量比一般平坦地形下垫面的大。Abstract: Untill now, there isn't any report on the atmospheric turbulence over tropical coastal area. By use of the observed data collected at Tianwei village of Hainan province in 1990, this paper analyses the turbulence characteristic values such as the velocity spectra and turbulence intensity. Most of these data are influenced by the cloud, and the stability parameter (L) and heat flux (wt) are not of daily variation in sunny days, but the turbulence energy and mean temperature are of normal daily variation. The base features of turbulent spectra are similar to those in the sunny days.The result shows that in the near surface layer over tropical coastal area, the turbulent behaviour is nearly consistent with the laws of local isotropy in the inertial subrange, the velocity spectra conform to the “-2/3”law in the Kolmogorov's similarity theory. Based on M O similarity theory, the relationship of the component turbulence intensities δi/U*(i=u ,v,w) and stability parameter Z/L has been studied, showing that the relationship displays the “1/3”law, but the turbulence intensity and energy are larger than that over plat and homogeneous terrain.
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Key words:
- Atmospheric turbulence /
- Turbulence intensity /
- Velocity spectra /
- Similarity theory
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