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Mapping floods due to Hurricane Sandy using NPP VIIRS and ATMS data and geotagged Flickr imagery

机译:使用NPP VIIRS和ATMS数据以及带有地理标签的Flickr影像来绘制飓风桑迪造成的洪水

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In this study, we present an approach to estimate the extent of large-scale coastal floods caused by Hurricane Sandy using passive optical and microwave remote sensing data. The approach estimates the water fraction from coarse-resolution VIIRS and ATMS data through mixed-pixel linear decomposition. Based on the water fraction difference, using the physical characteristics of water inundation in a basin, the flood map derived from the coarse-resolution VIIRS and ATMS measurements was extrapolated to a higher spatial resolution of 30 m using topographic information. It is found that flood map derived from VIIRS shows less inundated area than the Federal Emergency Management Agency (FEMA) flood map and the ground observations. The bias was mainly caused by the time difference in observations. This is because VIIRS can only detect flood under clear conditions, while we can only find some clear-sky data around the New York area on 4 November 2012, when most flooding water already receded. Meanwhile, microwave measurements can penetrate through clouds and sense surface water bodies under clear-or-cloudy conditions. We therefore developed a new method to derive flood maps from passive microwave ATMS observations. To evaluate the flood mapping method, the corresponding ground observations and the FEMA storm surge flooding (SSF) products are used. The results show there was good agreement between our ATMS and the FEMA SSF flood areas, with a correlation of 0.95. Furthermore, we compared our results to geotagged Flickr contributions reporting flooding, and found that 95% of these Flickr reports were distributed within the ATMS-derived flood area, supporting the argument that such crowd-generated content can be valuable for remote sensing operations. Overall, the methodology presented in this paper was able to produce high-quality and high-resolution flood maps over large-scale coastal areas.
机译:在这项研究中,我们提出了一种使用无源光学和微波遥感数据来估算飓风桑迪造成的大规模沿海洪灾程度的方法。该方法通过混合像素线性分解从粗分辨率VIIRS和ATMS数据估算水含量。根据水含量差异,利用盆地中淹水的物理特征,使用地形信息将由粗分辨率VIIRS和ATMS测量获得的洪水图外推到30 m的更高空间分辨率。发现从VIIRS得出的洪水图显示的淹没面积比联邦紧急事务管理局(FEMA)洪水图和地面观测更少。偏差主要是由观测的时间差异引起的。这是因为VIIRS只能在晴朗的条件下检测到洪水,而我们只能在2012年11月4日找到纽约地区附近的一些晴空数据,当时大多数洪水已经消退。同时,微波测量可以在晴朗或多云的条件下穿透云层并感知地表水体。因此,我们开发了一种从被动微波ATMS观测中得出洪水图的新方法。为了评估洪水测绘方法,使用了相应的地面观测资料和FEMA风暴潮洪水(SSF)产品。结果表明,我们的ATMS与FEMA SSF洪水区之间存在良好的一致性,相关系数为0.95。此外,我们将我们的结果与带有地理标记的Flickr贡献报告洪水进行了比较,发现这些Flickr报告中有95%分布在ATMS派生的洪水区域内,支持这样的论点,即这种人群产生的内容对于遥感行动可能是有价值的。总体而言,本文介绍的方法能够在大规模沿海地区绘制高质量和高分辨率的洪水地图。

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