Subgrid-Scale Dynamics of Water Vapour, Heat, and Momentum over a Lake     

Nikki Vercauteren  Elie Bou-Zeid  Marc B. Parlange  Ulrich Lemmin  Hendrik Huwald  John Selker  Charles Meneveau 《Boundary-Layer Meteorology》2008,128(2):205-228

We examine the dynamics of turbulence subgrid (or sub-filter) scales over a lake surface and the implications for large-eddy simulations (LES) of the atmospheric boundary layer. The analysis is based on measurements obtained during the Lake-Atmosphere Turbulent EXchange (LATEX) field campaign (August–October, 2006) over Lake Geneva, Switzerland. Wind velocity, temperature and humidity profiles were measured at 20 Hz using a vertical array of four sonic anemometers and open-path gas analyzers. The results indicate that the observed subgrid-scale statistics are very similar to those observed over land surfaces, suggesting that the effect of the lake waves on surface-layer turbulence during LATEX is small. The measurements allowed, for the first time, the study of subgrid-scale turbulent transport of water vapour, which is found to be well correlated with the transport of heat, suggesting that the subgrid-scale modelling of the two scalars may be coupled to save computational resources during LES.  相似文献   

Continuous Measurement of Number Concentrations and Elemental Composition of Aerosol Particles for a Dust Storm Event in Beijing   总被引：1，自引：0，他引：1  

ZHANG Renjian  HAN Zhiwei  SHEN Zhenxing  CAO Junji 《大气科学进展》2008,25(1):89-95

A continuous measurement of number size distributions and chemical composition of aerosol particles was conducted in Beijing in a dust storm event during 21-26 March 2001. The number concentration of coarse particles （ 〉2μm） increased more significantly than fine particles （ 〈2μm） during the dust storm due to dust weather, while the anthropogenic aerosols collected during the non-dust-storm period tended to be associated with fine particles. Elemental compositions were analyzed by using proton-induced X-ray emission （PIXE）. The results show that 20 elements in the dust storm were much higher than in the non-dust-storm period. The calculated soil dust concentration during the dust storm was, on average, 251.8μg m^-3, while it was only 52.1μg m^-3 on non-dust-storm days. The enrichment factors for Mg, A1, P, K, Ca, Ti, Mn, Fe, C1, Cu, Pb, and Zn show small variations between the dust storm and the non-dust-storm period, while those for Ca, Ni and Cr in the dust storm were much lower than those in the non-dust-storm period due to significant local emission sources. A high concentration and enrichment factor for S were observed during the dust storm, which implies that the dust particles were contaminated by aerosol particles from anthropogenic emissions during the long-range transport. A statistical analysis shows that the elemental composition of particles collected during the dust storm in Beijing were better correlated with those of desert soil colleted from desert regions in Inner Mongolia. Air mass back-trajectory analysis further confirmed that this dust storm event could be identified as streaks of dust plumes originating from Inner Mongolia.  相似文献   

Multi-Source Emission Determination Using an Inverse-Dispersion Technique     

Thomas K. Flesch  Lowry A. Harper  Raymond L. Desjardins  Zhiling Gao  Brian P. Crenna 《Boundary-Layer Meteorology》2009,132(1):11-30

Inverse-dispersion calculations can be used to infer atmospheric emission rates through a combination of downwind gas concentrations and dispersion model predictions. With multiple concentration sensors downwind of a compound source (whose component positions are known) it is possible to calculate the component emissions. With this in mind, a field experiment was conducted to examine the feasibility of such multi-source inferences, using four synthetic area sources and eight concentration sensors arranged in different configurations. Multi-source problems tend to be mathematically ill-conditioned, as expressed by the condition number κ. In our most successful configuration (average κ = 4.2) the total emissions from all sources were deduced to within 10% on average, while component emissions were deduced to within 50%. In our least successful configuration (average κ = 91) the total emissions were calculated to within only 50%, and component calculations were highly inaccurate. Our study indicates that the most accurate multi-source inferences will occur if each sensor is influenced by only a single source. A “progressive” layout is the next best: one sensor is positioned to “see” only one source, the next sensor is placed to see the first source and another, a third sensor is placed to see the previous two plus a third, and so on. When it is not possible to isolate any sources κ is large and the accuracy of a multi-source inference is doubtful.  相似文献   

三维交叉裂隙渗流传质特性数值模拟     

李博  黄嘉伦  钟振  邹良超 《岩土力学》2019,40(9):3670-3768

对交叉裂隙渗流传质特性的定量描述是研究整个裂隙网络渗透传质特性的基础。为真实模拟水流及溶质在三维交叉裂隙中的运移过程,首先通过三维轮廓仪获取天然岩石裂隙表面的形貌数据,再应用三维重构技术生成相应的三维交叉裂隙模型,随后求解Navier-Stokes方程,假定溶质运移满足Fick定律,模拟水流和溶质在三维交叉裂隙中的运移过程。通过对比粗糙裂隙模型与平行平板模型的模拟结果发现：粗糙度对流体的分布及流动状态存在显著的影响;不同进、出口工况下的流体流动及溶质运移状态亦表明：裂隙交叉的几何形貌会显著地影响溶质混合行为。这些结果表明,目前被广泛采用的平行平板模型在评估岩体内特别是交叉口的物质运移特性时将导致较大的偏差,在将来的研究中有必要针对裂隙交叉口的几何特征建立修正的模型以提高评估的准确性。  相似文献   

A depth average SPH model including μ(I) rheology and crushing for rock avalanches     

Alberto Longo  Manuel Pastor  Lorenzo Sanavia  Diego Manzanal  Miguel Martin Stickle  Chuan Lin  Angel Yague  Saeid Moussavi Tayyebi 《国际地质力学数值与分析法杂志》2019,43(5):833-857

Classical depth-integrated smoothed particle hydrodynamics (SPH) models for avalanches are extended in the present work to include a μ(I)− rheological model enriched with a fragmentation law. With this improvement, the basal friction becomes grain distribution dependent. Rock avalanches, where grain distribution tends to change with time while propagating, are the appropriate type of landslide to apply the new numerical proposal. The μ(I)− rheological models considered in the present work are those of Hatano and Gray, combined with two different fragmentation laws, a hyperbolic and a fractal-based law. As an application, Frank avalanche, which took place in Canada in 1903, is analyzed under the scope of the present approach, focusing in the influence of the rheological and fragmentation laws in the evolution of the avalanche.  相似文献   

GPS/BDS/GLONASS/Galileo多系统融合在中国区域的仿真分析     

徐炜  刘扬  严超  王涛  耿加伟 《测绘工程》2017,26(10)

通过STK软件对GPS、BDS、GLONASS、Galileo四个系统的星座结构进行仿真,并选择单系统与多系统组合定位的方式对中国区域内的可见卫星数、GDOP值和定位精度进行覆盖分析。结果表明,GPS/BDS/GLONASS/Galileo四系统组合定位在我国的GDOP值可达0.7~0.8,定位精度可达3~4m,优于其他方式的组合定位;同时四系统组合定位下的GDOP值降低,定位精度更好,GDOP值与定位精度的波动异常得到了抑制,导航定位的性能与稳定性也得到了相应的提升。  相似文献   

Android平台下的地形图图幅信息检索     

张红华 《测绘科学》2017,42(11)

针对当前移动端缺少快速、实时检索地形图图幅信息的系统,本文依据国家基本比例尺地形图分幅与编号标准,提出了基于Andriod平台的地形图图幅信息检索方法并编程实现了该系统。该系统实现的功能有:点所在图幅编号检索、图幅范围检索、地形图新旧编号的转换及区域范围内图幅编号集检索。此系统可应用于Andriod智能手机和平板电脑等移动设备。实验表明,本文的方法和系统执行效率能够基本满足移动用户实时检索地形图图幅信息的需求。  相似文献   

一次飞机积冰环境中的云微物理特征     

袁敏  黄敏松  段炼 《气象科技》2018,46(1):170-177

2014年3月12日利用机载粒子探头(DMT)对我国宜昌及周边地区的非降水云系进行了探测时发现了少量的飞机积冰,本文分析了积冰云层中云微物理量的分布特征。垂直平均分布表明,CAS、CIP和PIP粒子数浓度分别大于300个·cm~(-3)、1个·cm~(-3)和10~(-5)个·cm~(-3),粒子中值直径最大值分别为3μm、89μm和1389μm。谱分布表明,3650m高度重力碰并和凇附过程使得CIP和PIP粒子谱较宽,3650m以下谱宽较窄,粒子以凝结增长为主,大粒子和冰晶粒子主要是由高层下落造成。平飞观测统计表明,3350m的CAS和CIP粒子平均数浓度均大于3650m的值,但PIP粒子数浓度、粒子平均和最大中值直径则相反。平飞时间变化表明,3350m高度CAS粒子数浓度和直径大致呈反相关,3650m大云滴和冰雪晶粒子的数浓度和中值直径随时间波动较大。  相似文献   

Including Geological Uncertainty and Economic Analysis in a Rapid Simulation of Hydrocarbon Exploration     

Chungcharoen  E.  Fuller  J. David 《Natural Resources Research》1999,8(3):205-217

Manly's approximation method has been applied to hydrocarbon discovery process modeling in order to approximate the expected value and the standard deviation of the total discovery volume for a given exploratory effort. A major benefit of this method is that it allows the model to run much faster than the regular simulation method, yet it gives accurate results. This paper extends the benefit of Manly's approach by allowing the approximation method to incorporate the uncertainties in geological parameters that drive Manly's approximation, in order to provide an approximation of the complete distribution of total discovery volume that can result from exploration activity. In addition, it allows the model to include economic parameters into an evaluation of the economic worth of the results of exploration activity, producing distributions of net present value within a short period of time. The offshore Nova Scotia Shelf Basin is selected for demonstrating the methodology.  相似文献   

Gravitational potential changes of a spherically symmetric earth model caused by a surface load     

Wenke Sun  & Lars E. Sjöberg 《Geophysical Journal International》1999,137(2):449-468

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