大气科学学报
大氣科學學報
대기과학학보
JOURNAL OF NANJING INSTITUTE OF METEOROLOGY
2012年
2期
221-228
,共8页
姚菊香%李丽平%罗璇%杨玮%王盘兴
姚菊香%李麗平%囉璇%楊瑋%王盤興
요국향%리려평%라선%양위%왕반흥
准双周振荡%准一月振荡%Lanczos滤波器%Butterworth滤波器
準雙週振盪%準一月振盪%Lanczos濾波器%Butterworth濾波器
준쌍주진탕%준일월진탕%Lanczos려파기%Butterworth려파기
quasi-two-week oscillation%quasi-one-month oscillation%Lanczos filter%Butterworth filter
根据青藏高原大气热源季内振荡分析的实际需要,设计了适于提取准双周(10~20d)、准一月(20~40d)振荡的Lanczos滤波器(L.f.)。通过与Butterworth滤波器(B.f.)滤波效果的定量分析,确定了准双周、准一月L.f.窗宽参数l的临界值l0分别为24、46;当l≥l0时,L.f.滤波器性能全面优于B.f.。选用拉萨附近格点(90°E,30°N)的1950—2006年整层大气热源资料做了应用试验,结果表明,由l=121的L.f.得到的拉萨夏季准双周、准一月振荡分量质量可靠,可用于青藏高原大气热源季内振荡强度的年际差异和季内过程分析。
根據青藏高原大氣熱源季內振盪分析的實際需要,設計瞭適于提取準雙週(10~20d)、準一月(20~40d)振盪的Lanczos濾波器(L.f.)。通過與Butterworth濾波器(B.f.)濾波效果的定量分析,確定瞭準雙週、準一月L.f.窗寬參數l的臨界值l0分彆為24、46;噹l≥l0時,L.f.濾波器性能全麵優于B.f.。選用拉薩附近格點(90°E,30°N)的1950—2006年整層大氣熱源資料做瞭應用試驗,結果錶明,由l=121的L.f.得到的拉薩夏季準雙週、準一月振盪分量質量可靠,可用于青藏高原大氣熱源季內振盪彊度的年際差異和季內過程分析。
근거청장고원대기열원계내진탕분석적실제수요,설계료괄우제취준쌍주(10~20d)、준일월(20~40d)진탕적Lanczos려파기(L.f.)。통과여Butterworth려파기(B.f.)려파효과적정량분석,학정료준쌍주、준일월L.f.창관삼수l적림계치l0분별위24、46;당l≥l0시,L.f.려파기성능전면우우B.f.。선용랍살부근격점(90°E,30°N)적1950—2006년정층대기열원자료주료응용시험,결과표명,유l=121적L.f.득도적랍살하계준쌍주、준일월진탕분량질량가고,가용우청장고원대기열원계내진탕강도적년제차이화계내과정분석。
For the actual demand of analyzing intraseasonal oscillation of atmospheric heat source over the Tibetan Plateau,this paper devises Lanczos filter suitable for filtering quasi-two-week(10—20 d) and quasi-one-month(20—40 d) oscillations.By using the quantitative analysis and comparing with the filtering effect of Butterworth filter,the critical values l0 of window width parameter l of quasi-two week and quasi-one month Lanczos filter are determined as 24 and 46,respectively.The filtering capability of Lanczos filter is better than that of Butterworth filter when l is greater than or equal to l0.The whole atmospheric heat source data of the grid point(30°N,90°E) near Lhasa from 1950 to 2006 are used for test.Results indicate that,filtered by Lanczos filter with its parameter l being equal to 121,the quasi-two week and the quasi-one month components are dependable and can be used to analyze interannual difference and intraseasonal process of intraseasonal oscillation intensity of atmospheric heat source over the Tibetan Plateau.