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You have full text access to this contentA multi-temporal analysis of AMSR-E data for flood and discharge monitoring during the 2008 flood in Iowa (pages 2623–2634)

机译:您对IOWA洪水中的2008年洪水中的AMSR-E数据进行了全文,对AMSR-E数据进行了洪水和放电监控的多时间分析(第2623-2634页)

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The objective of this work is to demonstrate the potential of using passive microwave data to monitor flood and dischargeconditions and to infer watershed hydraulic and hydrologic parameters. The case study is the major flood in Iowa in summer2008. A new Polarisation Ratio Variation Index (PRVI) was developed based on a multi-temporal analysis of 37 GHz satelliteimagery from the Advanced Microwave Scanning Radiometer (AMSR-E) to calculate and detect anomalies in soil moistureand/or inundated areas. The Robust Satellite Technique (RST) which is a change detection approach based on the analysis ofhistorical satellite records was adopted. A rating curve has been developed to assess the relationship between PRVI valuesand discharge observations downstream. A time-lag term has been introduced and adjusted to account for the changing delaybetween PRVI and streamflow. Moreover, the Kalman filter has been used to update the rating curve parameters in near realtime. The temporal variability of the b exponent in the rating curve formula shows that it converges toward a constant value.A consistent 21-day time lag, very close to an estimate of the time of concentration, was obtained. The agreement betweenobserved discharge downstream and estimated discharge with and without parameters adjustment was 65 and 95%, respectively.This demonstrates the interesting role that passive microwave can play in monitoring flooding and wetness conditions andestimating key hydrologic parameters. Copyright  2011 John Wiley & Sons, Ltd.
机译:这项工作的目的是展示使用被动微波数据监测洪水和放电的潜力条件和推断流域水力和水文学参数。案例研究是夏季爱荷华州的主要洪水2008.基于37 GHz卫星的多时间分析,开发了一种新的偏振率变异指数(PRVI)从先进的微波扫描辐射计(AMSR-E)的图像计算和检测土壤水分的异常和/或淹没区域。基于分析的鲁棒卫星技术(RST)是一种改变检测方法采用了历史卫星记录。已经开发了评级曲线来评估PRVI值之间的关系和下游排出观察。已经引入并调整了一个时间滞后的术语,以占变化的延迟在PRVI和Streamflow之间。此外,卡尔曼滤波器已被用于更新近真实的额定值曲线参数时间。额定值曲线公式中B指数的时间可变性表明它朝向恒定值收敛。获得了一致的21天时间滞后,非常接近浓度时间的估计。协议观察到的下游和估计的放电分别为65%和95%。这证明了被动微波可以在监测洪水和湿度条件下发挥的有趣作用估算关键水文参数。版权所有2011 John Wiley&Sons,Ltd。

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