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首页> 外文期刊>Hydrology and Earth System Sciences >Aerodynamic roughness length estimation from very high-resolution imaging LIDAR observations over the Heihe basin in China
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Aerodynamic roughness length estimation from very high-resolution imaging LIDAR observations over the Heihe basin in China

机译:基于中国黑河流域超高分辨率成像激光雷达观测的空气动力学粗糙度长度估算

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Roughness length of land surfaces is an essential variable for theparameterisation of momentum and heat exchanges. The growing interest in theestimation of the surface turbulent flux parameterisation from passiveremote sensing leads to an increasing development of models, and the commonuse of simple semi-empirical formulations to estimate surface roughness.Over complex surface land cover, these approaches would benefit from thecombined use of passive remote sensing and land surface structuremeasurements from Light Detection And Ranging (LIDAR) techniques. Followingearly studies based on LIDAR profile data, this paper explores the use ofimaging LIDAR measurements for the estimation of the aerodynamic roughnesslength over a heterogeneous landscape of the Heihe river basin, a typicalinland river basin in the northwest of China. The point cloud obtained frommultiple flight passes over an irrigated farmland area were used to separatethe land surface topography and the vegetation canopy into a DigitalElevation Model (DEM) and a Digital Surface Model (DSM) respectively. Thesetwo models were then incorporated in two approaches: (i) a strictlygeometrical approach based on the calculation of the plan surface densityand the frontal surface density to derive a geometrical surface roughness;(ii) a more aerodynamic approach where both the DEM and DSM are introduced ina Computational Fluid Dynamics model (CFD). The inversion of the resulting3-D wind field leads to a fine representation of the aerodynamic surfaceroughness. Examples of the use of these three approaches are presented forvarious wind directions together with a cross-comparison of results onheterogeneous land cover and complex roughness element structures.
机译:陆地表面的粗糙度长度是动量和热交换参数化的基本变量。越来越多的人希望通过被动遥感来估计地表湍流参数化,从而导致模型的开发不断增加,以及使用简单的半经验公式来估算地表粗糙度的普遍性。在复杂的地表覆盖率下,这些方法将受益于利用光探测与测距(LIDAR)技术进行被动遥感和陆地表面结构测量。在基于LIDAR剖面数据的早期研究之后,本文探索了使用成像LIDAR测量来估算黑河流域(中国西北部典型的内陆流域)的异质景观上的空气动力学粗糙度长度。通过多次灌溉农田上空飞行获得的点云分别用于将土地表面地形和植被冠层分离为数字高程模型(DEM)和数字表面模型(DSM)。然后将这两个模型以两种方法结合在一起:(i)基于计算平面表面密度和前表面密度以得出几何表面粗糙度的严格几何方法;(ii)引入了DEM和DSM的更符合空气动力学的方法计算流体动力学模型(CFD)。产生的3-D风场的倒置导致空气动力学表面粗糙度的精细表示。给出了针对不同风向使用这三种方法的示例,以及对不均匀土地覆盖和复杂粗糙度元素结构的结果的交叉比较。

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