水文
水文
수문
HYDROLOGY
2015年
4期
14-19
,共6页
李敏%林炳章%邵月红%陈宏%吴俊梅
李敏%林炳章%邵月紅%陳宏%吳俊梅
리민%림병장%소월홍%진굉%오준매
地区线性矩法%水文气象一致区%频率估计值%空间插值
地區線性矩法%水文氣象一緻區%頻率估計值%空間插值
지구선성구법%수문기상일치구%빈솔고계치%공간삽치
∶ regional L-moments analysis%hydrometeorological region%quantile estimation%spatial interpolation
地区线性矩法(Regional L-moments Analysis,RLMA)是目前最先进的频率估算方法之一,自20世纪90年代起被广泛应用于美国及其他一些国家的防洪设计标准的分析计算中;我国近年也在太湖流域暴雨频率分析中成功地采用推广了这一水文气象途径的频率计算方法,积累了实际经验。但是,由于地面雨量站点有限、资料长度有限以及站点空间分布的不均匀等问题,研究区中相邻水文气象一致区之间暴雨频率估算值会出现空间不连续性的现象,这个空间不一致的问题尚没有得到合理的解决。在简要介绍地区线性矩法推求频率估计值的基础上,着重讨论并介绍一种概念清楚、简单易操作的基于空间往返二次内插的校正方法,来解决频率估算值空间不连续的问题。这种空间内插平差主要通过构造一个与研究区实测站点控制面积相应分辨率的虚拟网格站网来实现。研究结果表明,经过平差后校正的研究区内各站点的频率估计值的经验频率与理论概率更加接近,频率估计值的空间分布也更加合理。
地區線性矩法(Regional L-moments Analysis,RLMA)是目前最先進的頻率估算方法之一,自20世紀90年代起被廣汎應用于美國及其他一些國傢的防洪設計標準的分析計算中;我國近年也在太湖流域暴雨頻率分析中成功地採用推廣瞭這一水文氣象途徑的頻率計算方法,積纍瞭實際經驗。但是,由于地麵雨量站點有限、資料長度有限以及站點空間分佈的不均勻等問題,研究區中相鄰水文氣象一緻區之間暴雨頻率估算值會齣現空間不連續性的現象,這箇空間不一緻的問題尚沒有得到閤理的解決。在簡要介紹地區線性矩法推求頻率估計值的基礎上,著重討論併介紹一種概唸清楚、簡單易操作的基于空間往返二次內插的校正方法,來解決頻率估算值空間不連續的問題。這種空間內插平差主要通過構造一箇與研究區實測站點控製麵積相應分辨率的虛擬網格站網來實現。研究結果錶明,經過平差後校正的研究區內各站點的頻率估計值的經驗頻率與理論概率更加接近,頻率估計值的空間分佈也更加閤理。
지구선성구법(Regional L-moments Analysis,RLMA)시목전최선진적빈솔고산방법지일,자20세기90년대기피엄범응용우미국급기타일사국가적방홍설계표준적분석계산중;아국근년야재태호류역폭우빈솔분석중성공지채용추엄료저일수문기상도경적빈솔계산방법,적루료실제경험。단시,유우지면우량참점유한、자료장도유한이급참점공간분포적불균균등문제,연구구중상린수문기상일치구지간폭우빈솔고산치회출현공간불련속성적현상,저개공간불일치적문제상몰유득도합리적해결。재간요개소지구선성구법추구빈솔고계치적기출상,착중토론병개소일충개념청초、간단역조작적기우공간왕반이차내삽적교정방법,래해결빈솔고산치공간불련속적문제。저충공간내삽평차주요통과구조일개여연구구실측참점공제면적상응분변솔적허의망격참망래실현。연구결과표명,경과평차후교정적연구구내각참점적빈솔고계치적경험빈솔여이론개솔경가접근,빈솔고계치적공간분포야경가합리。
Regional L-moments analysis (RLMA) is the most advanced method for hydrologic frequency analysis, which has been widely used for precipitation frequency analysis in the United States and some other countries since the 1990s. Recently in China, RLMA has been successfully applied to precipitation frequency analysis in the Taihu Lake Basin as a pilot study. However, due to the lack of the rainfall stations with sparse spatial distributions as well as the short data length, the precipitation quantiles show a spatial discontinuation between quantiles somewhere around some areas in between the homogeneous regions. This study mainly presents a meaningful and simple correction method based on spatial interpolation to solve the discontinuity by adjusting the draft quantiles. The annual maximum series at 96 stations with 20-year and longer of rainfall data from the Taihu Lake Basin in East-China were used for the study. The results of adjusted precipitation quantiles that had been obtained via the RLMA for the Taihu Lake Basin exhibit better reliablity expressed in relative error of the empirical frequency to the theoretical exceedance probability of the data, and a better spatial smoothing pattern shown as well.