协同MIKE11-KF的遥感河道流量数据同化OA
Remote sensing river discharge data assimilation with MIKE11-KF
为提高无资料中小河流流量的模拟精度,通过卫星影像(Sentinel系列及高分影像)反演河道水面宽度并估算初步流量,将其作为流量观测值,与MIKE11 模型模拟的流量数据利用卡尔曼滤波算法进行同化,将同化后的流量结果作为MIKE11 模型的更新输入,形成闭环迭代,从而持续修正MIKE11 模型误差,提高模拟精度.曲周县黄口闸段的验证结果表明,卡尔曼滤波算法数据同化后MIKE11 模型模拟流量的R2 为 0.820,纳什效率系数NSE 为 0.813,相对均方根误差RRMSE 为0.260,较同化前R2 提高了28.1%,NSE提升了 27.0%,RRMSE降低了 43.5%,有效提高了河道流量模拟精度.
To improve the simulation accuracy of flow in ungauged small and medium rivers,river surface widths were inverted,and preliminary discharges were estimated using satellite imagery(Sentinel series and high-resolution images).These estimated values were then used as observed flow data and assimilated with the flow data simulated by the MIKE11 model using the Kalman filter algorithm.The assimilated flow results were fed back as updated inputs to the MIKE11 model,forming a closed-loop iteration that continuously corrected model errors and enhanced simulation accuracy.Validation results from the Huangkou Gate section in Quzhou County show that after data assimilation with the Kalman filter algorithm,the MIKE11 model achieves an R2 of 0.820,an NSE of 0.813,and an RRMSE of 0.260 for simulated flow.Compared to pre-assimilation results,R2 increases by 28.1%,NSE improves by 27.0%,and RRMSE decreases by 43.5%,demonstrating effective improvement in river discharge simulation accuracy.
李宾;栾清华;李涛;赵长森;李毛毛
河海大学农业科学与工程学院||西安理工大学旱区水工程生态环境全国重点实验室河海大学农业科学与工程学院曲周县水利局河长制办公室北京师范大学水科学研究院北京师范大学水科学研究院
卡尔曼滤波MIKE11模型遥感数据河道流量多源数据同化
Kalman filterMIKE11 modelremote sensing datariver dischargemulti-source data assimilation
《河海大学学报(自然科学版)》 2026 (2)
18-27,10
国家自然科学基金面上项目(52279004,52379008)
评论