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首页> 外文期刊>ISPRS Journal of Photogrammetry and Remote Sensing >Modeling spatiotemporal patterns of understory light intensity using airborne laser scanner (LiDAR)
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Modeling spatiotemporal patterns of understory light intensity using airborne laser scanner (LiDAR)

机译:使用机载激光扫描仪(LiDAR)对地下光强度的时空模式进行建模

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摘要

This study described a spatiotemporally explicit 3D raytrace model to provide spatiotemporal patterns of understory light (light intensity in the forest floor and along the vertical gradient). The model was built based on voxels derived from LiDAR and field investigation data, geographical information (elevation and location), and solar position (azimuth and altitude angles). We calculated the distance (L, in meters) traveled by solar ray in the crowns based on the model, and then calibrated and verified the light attenuation function using L based on Beer's law. L and the ratio of below canopy light intensity to above canopy light intensity showed obviously exponential relationship, with R~2 = 0.94 and P < 0.05. Estimated and observed understory light intensities were obviously positively correlated, with R~2 = 0.92 and P < 0.01, and the estimated values were slightly lower than the observed values. The spatiotemporal patterns of the light intensity in the forest floor were mapped with the respect to the solar position, and these patterns represented the variations in the forest-shaded area. The spatial patterns of the light intensity along vertical gradient were also mapped, and they showed strong variations. We concluded that L could account for the complex patterns of understory light environment with respect to the geographical and solar position variations. The 3D raytrace model can be integrated with ecological or hydrological models to resolve several issues, such as plant succession and competition, soil evaporation, plant transpiration, and snow-melt in the forest.
机译:这项研究描述了一个时空显式的3D光线跟踪模型,以提供地下光的时空模式(林地和垂直梯度的光强度)。该模型是基于从LiDAR获得的体素和野外调查数据,地理信息(海拔和位置)以及太阳位置(方位角和高度角)构建的。我们基于该模型计算了太阳光线在冠中传播的距离(L,以米为单位),然后根据比尔定律使用L校准和验证了光衰减函数。 L与冠层下光强度与冠层上光强度的比呈明显的指数关系,R〜2 = 0.94,P <0.05。估计和观测到的林下光强呈明显正相关,R〜2 = 0.92,P <0.01,估计值略低于观测值。相对于太阳位置绘制森林地面光强的时空分布图,这些图案代表了森林阴影区域的变化。还绘制了沿垂直梯度的光强度的空间模式,并且显示出很强的变化。我们得出的结论是,L可以解释相对于地理位置和太阳位置变化而言,地下光环境的复杂模式。可将3D射线跟踪模型与生态或水文模型集成,以解决多个问题,例如植物演替和竞争,土壤蒸发,植物蒸腾作用和森林融雪。

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