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Characterization Of Influence Zones Of Simulated Droughts And Floods Of Water Bodies In A Floodplain

机译:滩区模拟干旱和水体洪水影响区的特征

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During flooding processes, randomly situated water bodies of varying sizes and shapes in a floodplain tend to self-organize. At high degrees of flooding intensity, water bodies contact together to form influence zones, which indicate the self-organized criticality of the flooding of water bodies. The characterization of water bodies and their influence zones provides useful insight into the geomorphic properties of floodplain terrains. In this paper, characterization of the influence zones of simulated droughts and floods of water bodies in a floodplain is performed. First, drought and flood simulations are implemented by performing morphological erosion and dilation, respectively, on water bodies using square kernels of increasing sizes. The level of droughting/flooding is indicated by the kernel size. The average areas of the influence zones of the generated simulated droughts and floods of water bodies are computed. It is observed that as the droughting level increases from 1 to 5, the average area of the influence zones of water bodies reduces due to the shrinking of water bodies. As the droughting level increases from 5 to 15, the average area of the influence zones of water bodies increases due the vanishing of small water bodies. Flooding causes an increase in the average area of the influence zones of water bodies due to the merging of adjacent water bodies. A power law relationship is observed between the average area of the influence zones of the simulated droughts/floods and the level of droughting/flooding. The scaling exponent of this power law, which is named as a fractal dimension, indicates the rate of change of average area of the influence zones of simulated droughts/floods of water bodies in a floodplain over varying levels of droughting/flooding.
机译:在洪水过程中,洪泛区中随机放置的大小和形状各异的水体趋向于自组织。在高洪水强度下,水体相互接触形成影响区,这表明水体的自组织临界状态。水体及其影响区的特征为洪泛区地形的地貌特性提供了有用的见识。本文对洪泛区中水体的模拟干旱和洪水影响区进行了表征。首先,干旱和洪水模拟是通过使用逐渐增大的方粒分别在水体上进行形态侵蚀和膨胀来实现的。干旱/洪水的程度由籽粒大小指示。计算生成的模拟干旱和水体洪水影响区的平均面积。可以看出,随着干旱水平从1增加到5,由于水体的收缩,水体影响区的平均面积减小。随着干旱水平从5增加到15,由于小水体的消失,水体影响区的平均面积增加。由于相邻水体的合并,洪水导致水体影响区域的平均面积增加。在模拟干旱/洪灾影响区的平均面积与干旱/洪灾程度之间观察到幂律关系。该幂律的标度指数,称为分形维数,表示在不同水平的干旱/洪水下,洪泛区中模拟的干旱/水体洪水影响区平均面积的变化率。

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