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1.
城市下垫面空气动力学参数的估算   总被引:29,自引:2,他引:29  
为了定量描述北京城市下垫面的空气动力学特征,为模式提供准确的下垫面参数.利用气象塔大气湍流观测资料,结合Martano(2000)由单层超声风速、温度资料估算非均匀下垫面空气动力学参数的方法,计算了中国科学院大气物理研究所气象塔附近的下垫面空气动力粗糙度z0和零平面位移d,即z0为1.75 m和d为40.12 m.该结果与前人研究成果的比较结果表明最近的8年内,该处的零平面位移和空气动力粗糙度明显增大,这与该塔周围城市建设状况吻合.  相似文献   

2.
北京市郊区及城区边缘的大气湍流结构特征   总被引:10,自引:2,他引:10       下载免费PDF全文
张霭琛  吕杰  张兵 《大气科学》1991,15(4):87-96
为了比较城市边缘地区和郊区大气边界层中湍流结构的差异,本文分析了1986年春、夏两季在北京市城市边缘地区和郊区两处大气湍流观测结果.结果表明,由于城市边缘地区的下垫表面具有较高数值的粗糙度,使其近地面层大气受到较强的动力影响,在其湍流速度分量谱曲线;无量纲化湍流速度分量标准偏差,σ_u/u*,σ_v/u*和σ_w/u*;以及无量纲化湍流耗散率φ_ε等湍流特征量在近中性层结条件下显示出与大气稳定度的关系比较微弱.  相似文献   

3.
广州市近地层大气的湍流微结构和谱特征   总被引:16,自引:1,他引:16       下载免费PDF全文
本文利用UVW脉动风速仪资料分析了广州市区近地层大气的湍流强度、相关系数、尺度和速度谱,并获得了不同稳定度条件下的速度谱模式.结果表明,城市近地层大气湍流在惯性副区接近局地各向同性、速度谱符合Kolmogorov相似理论;气流方向上下垫面粗糙度的增加,使沿海城市近地层大气湍流能量(特别是铅直方向)比平坦、均匀下垫面上的增加.  相似文献   

4.
近地层大气湍流微结构对比分析   总被引:2,自引:0,他引:2  
利用黑河资料分析了戈壁下垫面上的近地层湍流微结构,并与其他下垫面上的端流微结构进行比较。结果表明:黑河戈壁滩上的湍流微结构满足局地相似理论,且有不同于其他下垫面的湍流结构特征;横向湍强较强,大小与纵向湍强相当。对湍流进行多尺度分析发现,黑河地区湍流结构呈现明显的多尺度分布,湍涡尺度量级从10^-2到10^2不等; 相比于v方向,u方向上占主要地位的湍涡尺度较大,但是所占比例罗小;随着不稳定度增加,  相似文献   

5.
南沙海域近海层大气湍流结构及输送特征研究   总被引:21,自引:0,他引:21       下载免费PDF全文
本文根据南沙群岛渚碧礁的一次大气湍流观测资料,分析研究南沙海域的湍流热通量输送、方差相似性、风速各分量谱、温度谱及各湍流通量协谱等大气湍流结构和输送特征,并与陆地下垫面上的结果作了比较,得到了一些有关南沙海域大气湍流输送及湍流结构的新认识。  相似文献   

6.
曾剑  张强 《高原气象》2012,31(6):1539-1550
采用2008年7-9月观测的中国干旱-半干旱区试验观测协同与集成研究资料,选取12个测站(涵盖不同气候环境区的草地、农田、果林和森林等下垫面)比较分析了干旱-半干旱区的动力、热力和水汽粗糙度长度、总体输送系数、反照率以及土壤热传导率和热扩散率的夏季平均特征,并与陆面模式的理论参考值进行了对比。结果表明,植被下垫面的水、热特性和植被高度对主要陆面参数有重要影响,但植被下垫面的土壤热传导率和扩散率与下垫面类型之间无明显关系。动力学粗糙度长度与下垫面的植被高度呈正相关关系,无论是稳定还是不稳定层结下,动量拖曳系数都随着植被高度的增大而增大,而反照率随植被高度的增加而降低。在研究区的下垫面中,草地下垫面动力学粗糙度长度的实测值比模式理论参考值偏小,但农田和果林下垫面的实测值比理论参考值偏大;草地下垫面动量拖曳系数理论的参考值比实测值高,但其他下垫面的实测值高于理论参考值;实测反照率处于可见光反照率和近红外光反照率之间,但反照率的理论参考值比实测值偏高。  相似文献   

7.
天津市郊大气边界层湍谱特征分析   总被引:10,自引:2,他引:10  
王存忠  曹文俊 《气象学报》1994,52(4):484-492
用1990年7月在天津市郊的观测资料,计算了风速谱、温度谱及动量和热量通量的协谱。结果表明,市郊下垫面上的大气湍流谱特征与平坦地形上得到的典型结果基本一致,但满足各向同性的湍流尺度似乎比在平坦地形上的略大,谱的峰值频率区域略窄,谱的低频区(含能区)特征与平坦地形上的情况也不同。  相似文献   

8.
引入通量footprint分析方法,结合广西白龙核电厂拟建厂址的湍流实测资料,分析了观测站点不同方向上的通量footprint,并由此确定了水平扩散尺度及水平扩散时间,最终估算了水平扩散参数。与环境评价导则中推荐的扩散时间计算所得的水平扩散参数进行了对比分析。结果表明,离岸流的扩散参数比向岸流大,有利于湍流扩散,从而证明扩散参数具有偏保守性和局地扩散的特性。分析表明,footprint方法在湍流扩散参数分析中具有实际的应用价值。  相似文献   

9.
热带沿海近地层大气的湍流结构和谱特征   总被引:5,自引:1,他引:5  
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  相似文献   

10.
长江三角洲常熟地区近地层湍流特征的研究   总被引:3,自引:0,他引:3  
利用1999年5~9月长江三角洲常熟地区的湍流脉动观测资料,分析了该地区感热、潜热和动量通量的日变化以及湍流强度和湍流谱特征,结果表明该地区各能量的日变化与常见情况相同,白天潜热通量的输送占主导地位,感热通量比潜热小得多,且湍流的日变化与天气的关系非常密切,晴天比阴天要大得多.湍流强度和湍流谱的分析结果表明,在近中性条件下,常熟地区各方向湍流强度接近典型平坦下垫面的值.非中性条件下,垂直方向规一化标准差与稳定度的关系都较好地满足1/3次幂定律,水平方向没有垂直方向上的规律好,特别是稳定条件下,数据点分散性大;各风速分量谱在高频段满足理论上的-2/3次幂定律,纵向和垂直方向速度谱的峰值频率与典型平坦下垫面上的结果一致.总体输送系数CD、CH与稳定度的关系密切,随稳定度增加有减小的趋势.  相似文献   

11.
不同下垫面上近地层湍流的多尺度属性研究   总被引:6,自引:2,他引:4  
文中利用统计和多尺度分析方法分析了几种复杂下垫面情况下的风、温湍流脉动观测资料 ,结果表明 :下垫面结构的差异明显地影响湍流量 ,如 :戈壁地区的热力作用明显大于雪面和城郊面 ,表现在湍流时间尺度上也明显地大于雪面和城郊面。但复杂下垫面下的湍谱在惯性区仍满足“- 23”次律 ;多尺度方法研究湍流 ,可以更简捷地分析湍流的多尺度结构及其在湍流输送中的作用。由此可看出 ,多尺度方法是发展湍流统计理论的一种有效工具。  相似文献   

12.
Artificial neural network (ANN) modeling has been performed to predict turbulent boundary layer characteristics for rough terrain based on experimental tests conducted in a boundary-layer wind tunnel to simulate atmospheric boundary layer using passive roughness devices such as spires, barriers, roughness elements on the floor, and slots in the extended test section. Different configurations of passive devices assisted to simulate urban terrains. A part of the wind tunnel test results are used as training sets for the ANN, and the other part of the test results are used to compare the prediction results of the ANN. Two ANN models have been developed in this study. The first one has been used to predict mean velocity, turbulence intensity, and model length scale factor. Results show that ANN is an efficient, accurate, and robust modeling procedure to predict turbulent characteristics of wind. In particular, it was found that the ANN-predicted wind mean velocities are within 4.7%, turbulence intensities are within 6.2%, and model length scale factors are within 3.8% of the actual measured values. In addition, another ANN model has been developed to predict instantaneous velocities that enables calculating the power spectral density of longitudinal velocity fluctuations. Results show that the predicted power spectra are in a good agreement with the power spectra obtained from measured instantaneous velocities.  相似文献   

13.
In this paper, turbulent data obtained from the Damxung site during the Secondary Tibetan Plateau Science Experiment (TIPEX) in 1998 are used to study the characteristics of the turbulent spectra, turbulence transport, and the dissipation rates of turbulent kinetic energy, temperature variance, and humidity variance in the middle area of the Tibetan Plateau. The turbulent spectra of wind velocity, potential temperature, and humidity satisfy the-2/3 power law in the high frequency range. Horizontal transportation of heat and water vapor is negligible compared with vertical transportation under strong unstable conditions, and as the stability parameter z/L increases (where z is the observational height, and L is the Monin Obukhov length), horizontal transportation becomes dominant under near-neutral, neutral, and stable conditions. The non-dimensional temperature and humidity variances are 20% less than the temperature and humidity gradient variances. These deficits appear to increase as the absolute stability parameter increases. Moreover, the effects of turbulence transportation and pressure variance exist throughout the entire stability region.  相似文献   

14.
In view of the absence or insufficiency of tropical cyclone(TC) turbulence parameters in current design standards of wind turbines, in this paper, TC turbulence parameter models with roughness length involved are developed based on six landfall TCs observed from meteorological towers located on various underlying surfaces, so as to provide references for the wind turbine design under TC conditions. Firstly, the roughness length values are examined in order to reduce the effect on turbulence parameters of the various underlying surfaces. On this basis, the reference turbulence intensity is normalized by the roughness length. The related turbulence parameters are parameterized, including the turbulence standard deviation and the turbulence spectrum; and the turbulence parameters available under TC conditions for turbulence turbine design are presented finally. Comparisons of the wind parameter models presented in this paper with those used in current turbine design standards suggest that the former can represent TC characteristics more accurately. In order to withstand TCs, we suggest that the turbulence parameter models recommended in this paper be included in future wind turbine design standards under TC conditions.  相似文献   

15.
Accurate predictions of turbulent characteristics in the atmospheric boundary layer (ABL) depends on understanding the effects of surface roughness on the spatial distribution of velocity, turbulence intensity, and turbulence length scales. Simulation of the ABL characteristics have been performed in a short test section length wind tunnel to determine the appropriate length scale factor for modeling, which ensures correct aeroelastic behavior of structural models for non-aerodynamic applications. The ABL characteristics have been simulated by using various configurations of passive devices such as vortex generators, air barriers, and slot in the test section floor which was extended into the contraction cone. Mean velocity and velocity fluctuations have been measured using a hot-wire anemometry system. Mean velocity, turbulence intensity, turbulence scale, and power spectral density of velocity fluctuations have been obtained from the experiments for various configuration of the passive devices. It is shown that the integral length scale factor can be controlled using various combinations of the passive devices.  相似文献   

16.
杨礼荣  任阵海 《高原气象》1990,9(4):382-387
本文利用100m~3系留气艇携带超声风温仪在复杂的盆地地形上空对1000m以下大气进行观测所获得的资料,研究小风稳定条件下大气边界层湍流结构特征。结果表明,在双对数坐标中,纵向速度u谱,垂直速度w谱,温度T谱在惯性区均遵循Kolmogorov的-2/3次律;横向速度V谱有其特殊的情形;协谱uw,wT及近地层的uT协谱在惯性区服从-4/3次律。和平坦、均一、开阔下垫面不同的是谱的峰值频率向高频移动,且没有发现近地层具有的谱峰随高度的明显变化关系。  相似文献   

17.
In this paper,the data chosen from measurements by supersonic anemometers in Tongxian County of Beijing in1990 are used to study characteristics of turbulence spectra in precipitation weather.Some turbulence parameters such asturbulence intensity,heat and momentum fluxes,friction velocity,M-O length and stability parameter are calculatedand their dependence on turbulence spectra in different stability conditions are analyzed.Some encouraging results areobtained and compared with others' results.  相似文献   

18.
In this paper,the data chosen from measurements by supersonic anemometers in Tongxian County of Beijing in 1990 are used to study characteristics of turbulence spectra in precipitation weather.Some turbulence parameters such as turbulence intensity,heat and momentum fluxes,friction velocity,M-O length and stability parameter are calculated and their dependence on turbulence spectra in different stability conditions are analyzed.Some encouraging results are obtained and compared with others' results.  相似文献   

19.
With a focus towards developing multiscale capabilities in numerical weather prediction models, the specific problem of the transition from the mesoscale to the microscale is investigated. For that purpose, idealized one-way nested mesoscale to large-eddy simulation (LES) experiments were carried out using the Weather Research and Forecasting model framework. It is demonstrated that switching from one-dimensional turbulent diffusion in the mesoscale model to three-dimensional LES mixing does not necessarily result in an instantaneous development of turbulence in the LES domain. On the contrary, very large fetches are needed for the natural transition to turbulence to occur. The computational burden imposed by these long fetches necessitates the development of methods to accelerate the generation of turbulence on a nested LES domain forced by a smooth mesoscale inflow. To that end, four new methods based upon finite amplitude perturbations of the potential temperature field along the LES inflow boundaries are developed, and investigated under convective conditions. Each method accelerated the development of turbulence within the LES domain, with two of the methods resulting in a rapid generation of production and inertial range energy content associated to microscales that is consistent with non-nested simulations using periodic boundary conditions. The cell perturbation approach, the simplest and most efficient of the best performing methods, was investigated further under neutral and stable conditions. Successful results were obtained in all the regimes, where satisfactory agreement of mean velocity, variances and turbulent fluxes, as well as velocity and temperature spectra, was achieved with reference non-nested simulations. In contrast, the non-perturbed LES solution exhibited important energy deficits associated to a delayed establishment of fully-developed turbulence. The cell perturbation method has negligible computational cost, significantly accelerates the generation of realistic turbulence, and requires minimal parameter tuning, with the necessary information relatable to mean inflow conditions provided by the mesoscale solution.  相似文献   

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