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Implications of boreal forest stand characteristics for X-band SAR flood mapping accuracy

机译:北方林分特征对X波段SAR洪水测绘精度的影响

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Synthetic aperture radar (SAR) enables the mapping of flooding over large areas, regardless of cloud and weather conditions. Simplified classification approaches based on threshold levels of backscattering intensity are typical in operational flood monitoring. Backscattering intensity from floods over open non-forested areas is typically lower, whereas backscatter from forest floods is higher compared to non-flooded areas. However, distinction of flooded areas from non-flooded surface in semi-forested areas with low canopy closure (CC) or low tree height (TH) is expected to be difficult due to confounding effects of the different scattering mechanisms. The aim of this study was to investigate X-band SAR backscattering in flooded boreal forests with varying TH and CC, and to quantify in which cases floods would be difficult to detect with typical threshold-based classification methods. To further understand the SAR signal behavior in flooded forests, the total backscatter was modeled using the HUT (Helsinki University of Technology) semi-empirical forest backscattering model. HH-polarized Cosmo Sky-Med acquisitions from four different locations in Finland were analyzed against airborne LiDAR based forest data, ground observations and a high resolution digital elevation model. Floods were well detected in open areas and dense forests. However, as hypothesized, when TH was higher than zero but lower than 4-5 m, or when CC was higher than zero but lower than 15-20%, the detection was less successful. TH was found to have slightly more influence on the capability of X-band SAR to detect floods than CC. In our four test areas, namely Kittila, Kolari, Pudasjarvi and Evo, 853%, 89.1%, 82.7% and 73.9% of the total floods were detected, respectively, by a simple threshold value method. The model was able to successfully estimate the different backscattering components of the flooded forests in Kittila and Pudasjarvi, where the number of observations from all forest conditions was sufficient. (C) 2016 Elsevier Inc. All rights reserved.
机译:合成孔径雷达(SAR)可以绘制大面积洪水的地图,而不受云和天气条件的影响。在运营洪水监控中,通常采用基于反向散射强度阈值水平的简化分类方法。在空旷的非森林地区,洪水造成的后向散射强度通常较低,而与非洪灾区相比,森林洪水造成的后向散射强度较高。然而,由于不同散射机制的混杂效应,预计很难将低盖度(CC)或低树高(TH)的半森林地区的水淹区与非水淹区区分开。这项研究的目的是调查TH和CC变化的北方水淹森林中的X波段SAR反向散射,并量化在哪些情况下使用典型的基于阈值的分类方法难以检测到洪水。为了进一步了解淹没森林中的SAR信号行为,使用HUT(赫尔辛基工业大学)半经验森林反向散射模型对总反向散射进行了建模。针对基于机载LiDAR的森林数据,地面观测和高分辨率数字高程模型,分析了在芬兰四个不同地点的HH极化Cosmo Sky-Med采集数据。在空旷地区和茂密的森林中很好地检测到洪水。但是,如假设的那样,当TH大于零但小于4-5 m时,或当CC大于零但小于15-20%时,检测不太成功。发现TH对X波段SAR检测洪水的能力的影响比CC稍大。在我们的四个测试区域,即基蒂拉,科拉里,普达斯贾维和埃沃,通过简单的阈值方法分别检测到洪水的853%,89.1%,82.7%和73.9%。该模型能够成功地估计基蒂拉和普达斯贾尔维的淹没森林的不同反向散射成分,而从所有森林条件中观察到的数量都足够。 (C)2016 Elsevier Inc.保留所有权利。

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