河海大学学报(自然科学版)
河海大學學報(自然科學版)
하해대학학보(자연과학판)
JOURNAL OF HOHAI UNIVERSITY (NATURAL SCIENCES)
2014年
2期
124-129
,共6页
刘开磊%姚成%李致家%阚光远%包红军
劉開磊%姚成%李緻傢%闞光遠%包紅軍
류개뢰%요성%리치가%감광원%포홍군
水动力学模型%模型实时校正%误差自回归方法%Kalman滤波算法%K最近邻算法
水動力學模型%模型實時校正%誤差自迴歸方法%Kalman濾波算法%K最近鄰算法
수동역학모형%모형실시교정%오차자회귀방법%Kalman려파산법%K최근린산법
hydrodynamic model%real-time correction%error autoregressive model%Kalman filtering algorithm%K-nearest neighbor algorithm
选择典型的实时校正方法:传统的误差自回归、基于K最邻近算法( KNN )的非参数校正及基于Kalman滤波的多断面校正法,并以Kalman滤波与KNN结合构造综合方法,以淮河流域吴家渡-小柳巷区间作为试验河段,构建一维水动力学模型并与实时校正方法联合应用。简要介绍这4种方法的原理与模型构建方法,然后对比分析各种方法的模拟结果,尤其对模拟洪峰稳定性、峰现时间、峰现误差等进行比较,认为前3种基本方法均能在相当长的预见期内提高洪水的预报精度,而综合法实时校正法对洪峰部位的模拟更为稳定可靠、总体效果更好,更适合预报校正工作的需要。
選擇典型的實時校正方法:傳統的誤差自迴歸、基于K最鄰近算法( KNN )的非參數校正及基于Kalman濾波的多斷麵校正法,併以Kalman濾波與KNN結閤構造綜閤方法,以淮河流域吳傢渡-小柳巷區間作為試驗河段,構建一維水動力學模型併與實時校正方法聯閤應用。簡要介紹這4種方法的原理與模型構建方法,然後對比分析各種方法的模擬結果,尤其對模擬洪峰穩定性、峰現時間、峰現誤差等進行比較,認為前3種基本方法均能在相噹長的預見期內提高洪水的預報精度,而綜閤法實時校正法對洪峰部位的模擬更為穩定可靠、總體效果更好,更適閤預報校正工作的需要。
선택전형적실시교정방법:전통적오차자회귀、기우K최린근산법( KNN )적비삼수교정급기우Kalman려파적다단면교정법,병이Kalman려파여KNN결합구조종합방법,이회하류역오가도-소류항구간작위시험하단,구건일유수동역학모형병여실시교정방법연합응용。간요개소저4충방법적원리여모형구건방법,연후대비분석각충방법적모의결과,우기대모의홍봉은정성、봉현시간、봉현오차등진행비교,인위전3충기본방법균능재상당장적예견기내제고홍수적예보정도,이종합법실시교정법대홍봉부위적모의경위은정가고、총체효과경호,경괄합예보교정공작적수요。
Three typical real-time correction methods, including the traditional error autoregressive method, the nonparametric correction method based on the K-nearest neighbor ( KNN ) , and the multi-cross section correction method based on Kalman filtering, as well as a combination of the KNN method and the Kalman filtering method were used in combination with a one-dimensional hydrodynamic model for flood forecasting and real-time correction in the Wujiadu-Xiaoliuxiang reach of the Huaihe Basin. The principles and construction methods of the four methods are briefly introduced, and a comparative analysis of their simulation results, especially of the stability of the flood peak, the time of occurrence of the flood peak, and the error of occurrence of the flood peak, is conducted. The conclusions are as follows: the three basic methods can improve the accuracy of flood forecasting over quite a long forecast period, and the combination method is more effective and reliable for flood peak simulation, and is more applicable to forecast correction.