地球物理学报
地毬物理學報
지구물이학보
2001年
1期
31-39
,共9页
江剑民%Klaus Fraedrich%邹耀仁
江劍民%Klaus Fraedrich%鄒耀仁
강검민%Klaus Fraedrich%추요인
扫描式t检验%多尺度突变现象%尼罗河水位
掃描式t檢驗%多呎度突變現象%尼囉河水位
소묘식t검험%다척도돌변현상%니라하수위
阐明了将检测两子样本平均值之差的学生氏t检验推广到对多尺度突变现象进行扫描式检测的计算方法;对于t检验要求序列独立的限制,引用了初步的订正方法;还给出了检测两个序列间多尺度突变相干性的计算公式.扫描式t检验不仅具有相当于子波变换检测多尺度突变现象的功能,而且解决了子波变换检测突变时缺少临界值的问题.由于t统计量包含有二阶矩均方差,它不能像子波变换那样作为分解工具,但检测的尺度参数也就不必局限于2的整数幂,因而可以进行扫描式检测.应用于尼罗河年最高与最低水位历史序列(AD622—1470),能较客观和精确地检测出两序列在某些尺度上的相干性(同步或反位相)变化;并由此重新划分了该流域几十年至百余年时间尺度的相对干湿期.结果与目前查阅到的埃及灾荒历史记载相吻合.
闡明瞭將檢測兩子樣本平均值之差的學生氏t檢驗推廣到對多呎度突變現象進行掃描式檢測的計算方法;對于t檢驗要求序列獨立的限製,引用瞭初步的訂正方法;還給齣瞭檢測兩箇序列間多呎度突變相榦性的計算公式.掃描式t檢驗不僅具有相噹于子波變換檢測多呎度突變現象的功能,而且解決瞭子波變換檢測突變時缺少臨界值的問題.由于t統計量包含有二階矩均方差,它不能像子波變換那樣作為分解工具,但檢測的呎度參數也就不必跼限于2的整數冪,因而可以進行掃描式檢測.應用于尼囉河年最高與最低水位歷史序列(AD622—1470),能較客觀和精確地檢測齣兩序列在某些呎度上的相榦性(同步或反位相)變化;併由此重新劃分瞭該流域幾十年至百餘年時間呎度的相對榦濕期.結果與目前查閱到的埃及災荒歷史記載相吻閤.
천명료장검측량자양본평균치지차적학생씨t검험추엄도대다척도돌변현상진행소묘식검측적계산방법;대우t검험요구서렬독립적한제,인용료초보적정정방법;환급출료검측량개서렬간다척도돌변상간성적계산공식.소묘식t검험불부구유상당우자파변환검측다척도돌변현상적공능,이차해결료자파변환검측돌변시결소림계치적문제.유우t통계량포함유이계구균방차,타불능상자파변환나양작위분해공구,단검측적척도삼수야취불필국한우2적정수멱,인이가이진행소묘식검측.응용우니라하년최고여최저수위역사서렬(AD622—1470),능교객관화정학지검측출량서렬재모사척도상적상간성(동보혹반위상)변화;병유차중신화분료해류역궤십년지백여년시간척도적상대간습기.결과여목전사열도적애급재황역사기재상문합.
A scanning t test of multi-scale abrupt changes is introduced byextending the student t test,which detects the difference between two subsample means. It is shown that this algorithm has not only the capacity similar to Haar wavelet transform coefficient W(a,b) for detection of multi-scale abrupt changes,but also gives the statistic significance threshold,which the wavelet analysis can not do. The subsample size n (comparative to the scale parameter a in W(a,b)) of the statistic t(n,j) may vary successively without limitation of integer power of 2 as in the wavelet transform for a discrete series,so that the algorithm may detect any longer signal series like a scanner. However,this algorithm is not a decomposition tool because the second momentum,the variance,is involved. In addition,a correction to the Effective Degrees of Freedom (Ef) of t test is adopted for the dependency of an observation series to be detected. A coherence detection of abrupt changes between two signal series is carried out. The results of an application to historic series (AD622-1470) of the maximum and minimum flood levels of the Nile River reveal objectively that there appears some abrupt changes in phase and out of phase on certain scales between the two series. The relative dry and wet phases on around 0.5—1.5 century scale are further repartitioned following this detection. And these dry/wet phases coincide better with historic records of catastrophe in Egypt found so far and are some improvements upon previous researches.