首页|基于Noah LSM的河套灌区土壤含水量同化研究

基于Noah LSM的河套灌区土壤含水量同化研究

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土壤含水量是灌区水资源管理研究中的关键参量,获得时空连续的可靠土壤含水量对灌区水资源管理意义重大.河套灌区是全国三大灌区之一,目前在该区域还没有开展时空连续土壤含水量的同化实验.本文利用地面实测单点土壤含水量数据和遥感反演区域土壤含水量数据,基于Noah LSM模型和集合卡尔曼滤波(EnKF)算法的同化方案实现了河套灌区时空连续土壤含水量的单点和区域模拟,并对比分析了同化结果和模型模拟结果.单点同化实验显示,同化结果和模型模拟结果均能反馈出强降雨中的土壤含水量变化,且模型模拟也能较好反应实测值变化,但同化结果比起模型结果更另接近实测值..区域同化实验表明,模型模拟土壤含水量的空间变异性时效果较差,同化结果能明显改善这个问题,整体模拟结果更接近于遥感反演的土壤含水量值.
Research on Soil Moisture Assimilation Based on Noah LSM in Hetao Irrigation District
Soil moisture is the key support to water resources management.It's meaningful for water resources management when obtaining available spatio-temporal continuous soil moisture.Hetao irrigation district is one of top three irrigation districts in China,in which there are no data-assimilation experiments to conduct in the aim of obtaining available spatio-temporal continuous soil moisture.This study uses observed point-scale soil moisture data on ground and region-scale soil moisture data by Remote Sensing to achieve modeling spatio-temporal continuous soil moisture in Hetao irrigation district based on Noah LSM and the Ensemble Kalman Filter(EnKF) algorithm.Then we analyzes and compares the results calculated by data-assimilation method and Noah model.Point-scale experiment shows results calculated by data-assimilation method and Noah model can both feedback the dramatic rainfall' influence and the former results are more close to ground observed soil moisture.Region-scale experiment illustrates that results calculated by Noah model represents worse spatial variability of soil moisture,which is obviously better showing by results calculated by data-assimilation method.Results calculated by data-assimilation method are more close to observed soil moisture by Remote Sensing.

soli moisturedata assimilationland surface process modelwater resources management in irrigation districtremote sensing

朱鹤、赵红莉、蒋云钟

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中国水利水电科学研究院水资源研究所,北京100038

土壤含水量 数据同化 陆面过程模型 灌区水资源管理 遥感

国家科技重大专项

082Y30B072 9001213/152 01

2016

科学技术与工程
中国技术经济学会

科学技术与工程

CSTPCD北大核心
影响因子:0.338
ISSN:1671-1815
年,卷(期):2016.16(10)
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