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首页> 外文期刊>Journal of hydrometeorology >Using the Back Propagation Neural Network Approach to Bias Correct TMPA Data in the Arid Region of Northwest China
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Using the Back Propagation Neural Network Approach to Bias Correct TMPA Data in the Arid Region of Northwest China

机译:利用反向传播神经网络方法对西北干旱地区的TMPA数据进行偏差校正

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摘要

Scarcity or unavailability of precipitation observation creates difficulties in hydrologic modeling of mountainous sections of the arid region of northwest China (34°-50°N, 72°-107°E). Tropical Rainfall Measuring Mission (TRMM) precipitation products may be a potential substitute, but they should be evaluated and corrected with ground observation data before application. In this paper, two TRMM Multisatellite Precipitation Analysis (TMPA) precipitation products were evaluated by gauge observations, using indices such as frequency bias index, probability of detection, false alarm ratio, relative mean bias, Nash-Sutcliffe efficiency, and correlation coefficient. Terrain variables were extracted from a digital elevation model, and their rotated principal components were determined to establish a stepwise regression model to adjustTMPA precipitation. Additionally, a back-propagation (BP) neural network was established to correct TMPA precipitation. The results showed thatTMPAhad an unsatisfactory detection ability in the study area for both precipitation occurrence and amount.TMPAprecipitation corrected by a stepwise regression method showed some improvement, but only the results forTRMM3B43 on a subregion scale were acceptable. The BP neural network method showed better results than the stepwise regression method, and both TRMM 3B42 and TRMM 3B43 corrected by the former method on a subregion scale could be acceptable. Both methods were spatial-scale dependent and showed better results on a subregion scale than on a larger scale.
机译:降水观测的稀缺或不可用给中国西北干旱地区(34°-50°N,72°-107°E)的山区水文模拟带来了困难。热带雨量测量任务(TRMM)降水产品可能是潜在的替代产品,但在使用前应先进行地面观测数据评估和校正。本文使用频率偏差指数,检测概率,误报率,相对平均偏差,纳什-萨特克利夫效率和相关系数等指标,通过量表观测评估了两种TRMM多卫星降水分析(TMPA)降水产物。从数字高程模型中提取地形变量,并确定它们的旋转主分量以建立逐步回归模型来调整TMPA降水量。此外,建立了反向传播(BP)神经网络以纠正TMPA降水。结果表明,TMPA在研究区的降水量和降水量检测能力均不令人满意。通过逐步回归法校正的TMPA降水量显示出一定的改善,但只有TRMM3B43在分区范围内的结果是可以接受的。 BP神经网络方法显示出比逐步回归方法更好的结果,并且在局部区域尺度上用前一种方法校正的TRMM 3B42和TRMM 3B43都是可以接受的。两种方法都依赖于空间尺度,并且在次区域尺度上显示出比更大尺度上更好的结果。

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