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Using SPOT and Aerial False-Color Infrared (fCIR) Imagery to Verify Floodplain Model Results in West Central Florida

机译:使用SPOT和航空伪彩色红外(fCIR)图像验证佛罗里达州中西部的洪泛区模型结果

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Tropical Storm Debby brought severe flooding to portions of southwestern Florida during the summer of 2012. Remotely-sensed images were collected to document the flooding and test the results of Hydrologic and Hydraulic (H & H) storm water models constructed by the Southwest Florida Water Management District (SWFWMD). One image, a satellite, multi-band SPOT image was provided to the SWFWMD by the Federal Emergency Management Agency (FEMA). This image was collected within 48 h of the storm event. The SWFWMD also contracted for a very high resolution (60 cm Ground Sample Distance (GSD)) fCIR image to be captured for selected watersheds in Citrus, Hernando and Pasco counties, the areas most impacted by the flooding. Modeled floodplain results were compared to remotely-sensed images that were georeferenced and analyzed using remote sensing techniques. The higher resolution fCIR images more clearly identified flooding for better comparison with modeled results. Although the fCIR images, which were collected three to four days after the storm event, under predicted the overall extent of the modeled floodplain, as the images could not confirm the presence of flooding in areas obscured by dense vegetation, they did consistently confirm both the location and shape of flooding simulated by the model. By using image analysis methods on the Near-Infrared (NIR) band of the fCIR image in conjunction with the Digital Elevation Model (DEM), however, it was possible to identify the extent of flooding in those obscured areas. Field surveys of high water elevations indicated that many locations had receded within hours of the storm event, limiting the ability of the fCIR image from capturing peak flood level in all areas. Overall, these remotely-sensed images provided a good validation of predicted flood levels for a design storm of the magnitude of Tropical Storm Debby.
机译:热带风暴戴比在2012年夏季向佛罗里达州西南部的部分地区带来了严重的洪灾。收集了遥感图像以记录洪水并测试了西南佛罗里达水管理公司构建的水文和水力(H&H)雨水模型的结果区(SWFWMD)。联邦紧急事务管理局(FEMA)向SWFWMD提供了一张图像,卫星多波段SPOT图像。该图像是在风暴事件发生后48小时内收集的。 SWFWMD还签订了非常高分辨率(60厘米地面采样距离(GSD))fCIR图像的合同,以便为受洪水影响最大的柑橘,埃尔南多和帕斯科县的选定集水区拍摄。将模拟的洪泛区结果与经过地理定位并使用遥感技术进行分析的遥感图像进行比较。分辨率更高的fCIR图像可以更清晰地识别出泛洪,以便更好地与建模结果进行比较。尽管在风暴事件发生后三到四天收集的fCIR图像虽然无法预测模型洪泛区的总体范围,但由于图像无法确定茂密植被所遮盖的区域中是否存在洪水,因此它们始终一致地确认了模型模拟的洪水位置和形状。但是,通过在fCIR图像的近红外(NIR)波段上使用图像分析方法,并结合数字高程模型(DEM),可以确定那些被遮盖区域的水浸程度。高水位的现场调查表明,暴风雨事件发生后数小时内,许多地点已经退缩,这限制了fCIR图像捕获所有地区洪峰的能力。总体而言,这些遥感图像很好地验证了热带风暴戴比级设计风暴的预测洪水位。

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