首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Use of airborne LiDAR and historical aerial photos for characterising the history of braided river floodplain morphology and vegetation responses
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Use of airborne LiDAR and historical aerial photos for characterising the history of braided river floodplain morphology and vegetation responses

机译:使用机载激光雷达和历史空中照片,以表征编织河洪泛区形态和植被反应的历史

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This paper combines synoptic airborne LiDAR data with historical aerial photos to reconstruct floodplain formation and relate this with vegetation patch characteristics on three different alpine braided rivers in France displaying a gradient of geomorphic activity (Bouinenc Drome Bes). LiDAR data were processed to extract understory topography and vegetation properties. Once combined with sequential aerial photographs for the dating of floodplain formation, they were used to establish the timing of channel incision associated with active channel narrowing. It has thus been possible not only to reconstruct the main incision periods following the end of the Little Ice Age, but also to show the geomorphic effect of floods on active channel widening, which was clearly modulated by sediment supply conditions. Well-developed floodplains with a predominance of mature vegetation units are associated with long-term narrowing and incision trajectories, whereas rivers maintaining a wide active channel over time show equi-diversity of floodplain vegetation units. The presence of shrub patches seems to be a good indicator of incision periods. A discriminant analysis using LiDAR-derived topographic and vegetation properties of floodplain patches as well as their age provided a validation of the expert-based mapping of physiognomic vegetation units (shrubland, sparse pioneer, dense pioneer, and post-pioneer units). This approach also provides insights into identification and interpretation of misclassifications and open new perspectives for exploring landscape ecolbgical trajectories and their controlling factors. (C) 2016 Elsevier B.V. All rights reserved.
机译:本文将舞台空气传播的LIDAR数据与历史空中照片结合在一起,以重建洪泛区的形成,并将其与法国三种不同的高山编织河上的植被补丁特征相关联,显示出几形活动的梯度(Bouinenc& dr; dr; bes)。加工LIDAR数据以提取较大的地形和植被属性。一旦结合连续的空中照片进行泛洪平面形成,它们用于建立与活动通道缩小相关的通道切口的时序。因此,不仅可以在小冰河时代结束后重建主切口期,而且还表明了通过沉积物供应条件清楚地调节了活性通道扩大的洪水的几何效果。发达于成熟植被单元的优势源于长期缩小和切口轨迹的洪泛平原,而维持宽活跃的通道随着时间的推移,河流的河流展示了洪泛平原植被单位的平衡。灌木斑块的存在似乎是切口期的良好指标。使用泛乐计划斑块的LiDAR衍生地形和植被特性的判别分析以及其年龄提供了基于专家的地理学植被单位(灌木丛,稀疏先驱,密集先驱和先驱单位)的验证。这种方法还提供了对错误分类和解释的见解,并开辟了探索景观生成轨迹及其控制因素的新观点。 (c)2016年Elsevier B.v.保留所有权利。

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