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Monitoring of flood in Gujarat region using AQUA AMSR-E derived surface soil moisture

机译:使用AQUA AMSR-E得出的地表土壤湿度监测古吉拉特邦地区的洪水

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摘要

AQUA AMSR-E L3 soil moisture data of 5 years (2002-06) were analyzed over Gujarat, India for flood analysis. We have used a threshold value (Gujarat 40% and Rajasthan desert 20%) for soil moisture to estimate flood affected area. Time series daily soil moisture data during flood period in Gujarat shows that soil moisture above threshold has been observed during 2004-06. The estimated flood area in Gujarat was 8418, 22618, 6313 sq. km in 2004, 05 and 06 respectively. Recent 2006 flood in Barmer, Rajasthan shows 7366 sq. km flood affected area with 20% as threshold soil moisture. The flood-area correlates well with rainfall data and surface soil moisture distribution. As the resolution of AMSR-E (60 km) is very poor, the area estimation is not so accurate. But the soil moisture trend clearly shows variation in flood affected area with days. The results from this method are to be compared with methods available using other data sets or techniques. Fixing a threshold value for soil moisture of a particular test site is also very important in the estimation of flood affected area.
机译:对印度古吉拉特邦5年(2002-06年)的AQUA AMSR-E L3土壤湿度数据进行了洪水分析。我们已使用土壤水分的阈值(古吉拉特邦40%,拉贾斯坦沙漠20%)来估算洪水影响面积。古吉拉特邦洪水期间的时间序列每日土壤水分数据显示,在2004-06年期间观测到土壤水分超过阈值。 2004、05和06年古吉拉特邦的估计洪灾面积分别为8418、22618、6313平方公里。拉贾斯坦邦巴默市(Barmer)最近发生的2006年洪水,显示受洪水影响的面积为7366平方公里,其中20%作为临界土壤湿度。洪水区与降雨数据和地表土壤水分分布密切相关。由于AMSR-E(60 km)的分辨率非常差,因此面积估计不太准确。但是,土壤水分趋势清楚地显示了受洪水影响的地区随天数的变化。该方法的结果将与使用其他数据集或技术可获得的方法进行比较。固定特定测试地点的土壤水分阈值对于评估洪水影响面积也非常重要。

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