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首页> 外文期刊>Hydrology and Earth System Sciences >Flood occurrence mapping of the middle Mahakam lowland area using satellite radar
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Flood occurrence mapping of the middle Mahakam lowland area using satellite radar

机译:利用卫星雷达绘制马哈卡姆邦中部低洼地区的洪水发生图

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摘要

Floodplain lakes and peatlands in the middle Mahakam lowland area are considered as ecologically important wetland in East Kalimantan, Indonesia. However, due to a lack of data, the hydrological functioning of the region is still poorly understood. Among remote sensing techniques that can increase data availability, radar is well-suitable for the identification, mapping, and measurement of tropical wetlands, for its cloud unimpeded sensing and night and day operation. Here we aim to extract flood extent and flood occurrence information from a series of radar images of the middle Mahakam lowland area. We explore the use of Phased Array L-band Synthetic Aperture Radar (PALSAR) imagery for observing flood inundation dynamics by incorporating field water level measurements. Water level measurements were carried out along the river, in lakes and in peatlands, using pressure transducers. For validation of the open water flood occurrence map, bathymetry measurements were carried out in the main lakes. A series of PALSAR images covering the middle and lower Mahakam area in the years 2007 through 2010 were collected. A fully inundated region can be easily recognized on radar images from a dark signature. Open water flood occurrence was mapped using a threshold value taken from radar backscatter of the permanently inundated river and lakes areas. Radar backscatter intensity analysis of the vegetated floodplain area revealed consistently high backscatter values, indicating flood inundation under forest canopy. We used those values as the threshold for flood occurrence mapping in the vegetated area.
机译:Mahakam低地中部的洪泛区湖泊和泥炭地被认为是印度尼西亚东加里曼丹省的重要生态湿地。但是,由于缺乏数据,对该地区的水文功能仍知之甚少。在可以提高数据可用性的遥感技术中,雷达由于其云不受阻碍的传感和昼夜操作,非常适合于热带湿地的识别,测绘和测量。在这里,我们旨在从中部马哈卡姆低地地区的一系列雷达图像中提取洪水范围和洪水发生信息。我们探索使用相控阵L波段合成孔径雷达(PALSAR)图像,通过结合野外水位测量来观察洪水泛滥动态。使用压力传感器在河流,湖泊和泥炭地中进行水位测量。为了验证开放水域洪水发生图,在主要湖泊进行了水深测量。收集了2007年至2010年一系列覆盖Mahakam中下部地区的PALSAR图像。雷达图像上的暗信号很容易识别出完全淹没的区域。使用从永久淹没的河流和湖泊区域的雷达反向散射中获取的阈值来绘制开放水域洪水发生的地图。植被泛滥区的雷达反向散射强度分析显示一致的较高反向散射值,表明森林冠层下洪水泛滥。我们将这些值用作植被区中洪水发生映射的阈值。

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