水力发电
水力髮電
수력발전
WATER POWER
2015年
2期
12-15,44
,共5页
游海林%徐力刚%刘桂林%吴永明%王晓龙%姜加虎
遊海林%徐力剛%劉桂林%吳永明%王曉龍%薑加虎
유해림%서력강%류계림%오영명%왕효룡%강가호
历年年均水位%Morlet小波%星子站%鄱阳湖
歷年年均水位%Morlet小波%星子站%鄱暘湖
력년년균수위%Morlet소파%성자참%파양호
mean annual water level fluctuation%Morlet wavelet%Xingzi Hydrological Station%Poyang Lake
运用Morlet连续复小波函数分析鄱阳湖星子水文站1953年~2012年历年年均水位变动的多时间尺度演变特征,并在水位变动的小波方差分析结果的基础上运用surfer8.0绘制出控制鄱阳湖历年年均水位演变的主周期趋势图。结果表明,鄱阳湖历年年均水位在不同时间尺度的分辨率条件下,其序列显现出不同的周期交替现象,演变过程中存在着25~32、19~23、8~15年以及3~7年4类时间尺度的周期变化规律;其变动存在3个较为明显的峰值,依次对应着28、22、5年的时间尺度;3类时间尺度具有较明显的局部化特征,前两个时间尺度上,年均水位变动的平均周期为19、15年左右,在5年时间尺度上,历年年均水位变动的频率变化较快,同时振荡行为也较明显。
運用Morlet連續複小波函數分析鄱暘湖星子水文站1953年~2012年歷年年均水位變動的多時間呎度縯變特徵,併在水位變動的小波方差分析結果的基礎上運用surfer8.0繪製齣控製鄱暘湖歷年年均水位縯變的主週期趨勢圖。結果錶明,鄱暘湖歷年年均水位在不同時間呎度的分辨率條件下,其序列顯現齣不同的週期交替現象,縯變過程中存在著25~32、19~23、8~15年以及3~7年4類時間呎度的週期變化規律;其變動存在3箇較為明顯的峰值,依次對應著28、22、5年的時間呎度;3類時間呎度具有較明顯的跼部化特徵,前兩箇時間呎度上,年均水位變動的平均週期為19、15年左右,在5年時間呎度上,歷年年均水位變動的頻率變化較快,同時振盪行為也較明顯。
운용Morlet련속복소파함수분석파양호성자수문참1953년~2012년력년년균수위변동적다시간척도연변특정,병재수위변동적소파방차분석결과적기출상운용surfer8.0회제출공제파양호력년년균수위연변적주주기추세도。결과표명,파양호력년년균수위재불동시간척도적분변솔조건하,기서렬현현출불동적주기교체현상,연변과정중존재착25~32、19~23、8~15년이급3~7년4류시간척도적주기변화규률;기변동존재3개교위명현적봉치,의차대응착28、22、5년적시간척도;3류시간척도구유교명현적국부화특정,전량개시간척도상,년균수위변동적평균주기위19、15년좌우,재5년시간척도상,력년년균수위변동적빈솔변화교쾌,동시진탕행위야교명현。
The mean annual water levels from 1953 to 2012 in Poyang Lake are selected as the study object, and the complex continuous Morlet wavelet is used to study the multi-time-scale variation characteristic of water level fluctuations. Based on the wavelet variances, the primary period trend graphs that control the mean annual water level fluctuations of Poyang Lake are drawn out. The results show that: (a) there are four cycle variations (i.e. years of 25-32, 19-23, 8-15 and 3-7) in mean annual water level fluctuations in Poyang Lake, and the strength and distribution of each cycle variation is different as well as the catastrophe point; (b) the mean annual water level fluctuations are mainly in the presence of three conspicuous peaks, which are in correspondence with the time scales of years of 28, 22 and 5 in Poyang Lake;and (c) each different time scale has apparently localized features, i.e. the mean water level fluctuation cycle is about 19 years in the 28-year time scale and about 15 years in the 22-year time scale, but the water level fluctuation changes more frequently and oscillates more significantly in the 5-year time scale.