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安徽省土壤湿度时空变化规律分析及遥感反演
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  • 英文篇名:Spatiotemporal analysis and remote sensing retrieval of soil moisture across Anhui Province,China
  • 作者:王青青 ; 张珂 ; 叶金印 ; 李致家
  • 英文作者:WANG Qingqing;ZHANG Ke;YE Jinyin;LI Zhijia;State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Hohai University;College of Hydrology and Water Recourses,Hohai University;Anhui Branch of China Meteorological Administration Training Centre;
  • 关键词:安徽省 ; 土壤湿度 ; 时空变化 ; 人工神经网络 ; 微波遥感 ; 土壤湿度卫星反演
  • 英文关键词:Anhui Province;;soil moisture;;spatiotemporal variability;;artificial neural network;;remote sensing;;satellite retrieval of soil moisture
  • 中文刊名:HHDX
  • 英文刊名:Journal of Hohai University(Natural Sciences)
  • 机构:河海大学水文水资源与水利工程科学国家重点实验室;河海大学水文水资源学院;中国气象局气象干部培训学院安徽分院;
  • 出版日期:2019-03-25
  • 出版单位:河海大学学报(自然科学版)
  • 年:2019
  • 期:v.47
  • 基金:国家重点研发计划(2016YFC0402701);; 国家自然科学基金(518679067);; 江苏省杰出青年基金(BK20180022)
  • 语种:中文;
  • 页:HHDX201902004
  • 页数:5
  • CN:02
  • ISSN:32-1117/TV
  • 分类号:24-28
摘要
为获取安徽省的土壤湿度时空信息,采用克里金法将站网实测多层土壤湿度数据插值为网格数据,分析其时空变化特征;进而建立遗传算法优化的BP(back propagation)神经网络模型进行土壤湿度反演。该模型以风云3B卫星的亮温数据为主要输入,训练后对该模型验证并进行预测。结果表明:安徽省土壤湿度月均值波动较频繁,淮北平原和大别山区较其他区域干燥;随着深度的增加,土壤湿度增大且季节和空间差异变小;所有分区平均模拟值与实测值的日序列相关性达到0. 605,均方根误差为0. 056 m~3/m~3,说明该模型能够较好地反演安徽省土壤湿度
        To obtain the spatiotemporal characteristics of soil moisture in Anhui Province,the Kriging method was firstly used to interpolate the in-situ observed and multilayer soil moisture to gridded data. Then,the spatiotemporal variability of soil moisture across this region was analyzed. A Back Propagation( BP) neural network optimized by the genetic algorithm was established to retrieve the soil moisture using the brightness temperature measured by the Fengyun 3 B satellite. The results show that soil moisture across Anhui Province shows high temporal fluctuations.And,the soil moisture in the Huaibei plain and the Dabie Mountains is lower than the other regions. As depth becomes deeper,soil moisture has a higher value with lower seasonal and horizontal variability. The correlation between retrieved and observed daily gridded values across the five sub-regions is 0.605,while the corresponding root mean square error is 0. 056 m~3/m~3. Clearly, the proposed retrieval algorithm is able to capture the spatiotemporal variability of soil moisture in Anhui Province.
引文
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