大气科学学报
大氣科學學報
대기과학학보
JOURNAL OF NANJING INSTITUTE OF METEOROLOGY
2012年
3期
342-349
,共8页
风速%均一性%直接检验方法%间接检验方法
風速%均一性%直接檢驗方法%間接檢驗方法
풍속%균일성%직접검험방법%간접검험방법
wind speed%homogeneity%direct test%indirect test
针对安徽省天长和宿松气象站建站至2010年逐年平均风速资料,分别利用直接检验方法和3种间接检验方法:标准正态均一检验(the standard normalhomogeneity test,SNHT)、惩罚最大t检验(the penalized maximal t test,PMTT)和惩罚最大F检验(the penalized maximal Ftest,PMFT),对这两个气象站逐年平均风速序列进行了均一性检验,并对不同检验方法的效果进行了对比分析。研究结果表明:1)站址迁移、观测场环境变化、仪器变更以及测风手段变化等均能对年平均风速序列的均一性产生影响,其中测风手段变化的影响最为明显。2)由于以气象台站观测记录为依据,直接检验得到的结果最为真实可信;此外SNHT、PMTT和PMFF方法对年平均风速序列的间断点均有一定的检验能力,但遗漏间断点的情况也比较明显。因而在年平均风速序列的均一性检验中,若气象台站观测记录相对较齐全,首先考虑采用直接检验,然后再考虑补充采用其他间接检验手段。
針對安徽省天長和宿鬆氣象站建站至2010年逐年平均風速資料,分彆利用直接檢驗方法和3種間接檢驗方法:標準正態均一檢驗(the standard normalhomogeneity test,SNHT)、懲罰最大t檢驗(the penalized maximal t test,PMTT)和懲罰最大F檢驗(the penalized maximal Ftest,PMFT),對這兩箇氣象站逐年平均風速序列進行瞭均一性檢驗,併對不同檢驗方法的效果進行瞭對比分析。研究結果錶明:1)站阯遷移、觀測場環境變化、儀器變更以及測風手段變化等均能對年平均風速序列的均一性產生影響,其中測風手段變化的影響最為明顯。2)由于以氣象檯站觀測記錄為依據,直接檢驗得到的結果最為真實可信;此外SNHT、PMTT和PMFF方法對年平均風速序列的間斷點均有一定的檢驗能力,但遺漏間斷點的情況也比較明顯。因而在年平均風速序列的均一性檢驗中,若氣象檯站觀測記錄相對較齊全,首先攷慮採用直接檢驗,然後再攷慮補充採用其他間接檢驗手段。
침대안휘성천장화숙송기상참건참지2010년축년평균풍속자료,분별이용직접검험방법화3충간접검험방법:표준정태균일검험(the standard normalhomogeneity test,SNHT)、징벌최대t검험(the penalized maximal t test,PMTT)화징벌최대F검험(the penalized maximal Ftest,PMFT),대저량개기상참축년평균풍속서렬진행료균일성검험,병대불동검험방법적효과진행료대비분석。연구결과표명:1)참지천이、관측장배경변화、의기변경이급측풍수단변화등균능대년평균풍속서렬적균일성산생영향,기중측풍수단변화적영향최위명현。2)유우이기상태참관측기록위의거,직접검험득도적결과최위진실가신;차외SNHT、PMTT화PMFF방법대년평균풍속서렬적간단점균유일정적검험능력,단유루간단점적정황야비교명현。인이재년평균풍속서렬적균일성검험중,약기상태참관측기록상대교제전,수선고필채용직접검험,연후재고필보충채용기타간접검험수단。
By using the direct homogeneity test (based on the observation data and the t test) and 3 in- direct homogeneity methods (including SNHT, PMTT and PMFT ), time series of annual mean wind speed at 2 meteorological stations,Tianchang and Susong,from 1957 to 2010,have been tested respec-tively. The results show that station relocation, observational environment change, instruments updating and measurements variation can all influence the homogeneity of the mean wind speed, and the impact of measurements updating is the most prominent factor. Because based on observation data from meteor-ological stations, the results of direct test is more reliable. However, SNHT, PMTT and PMFT are effec-tive in identifying the change-points, but the missing ratio is also of a high degree. Thus, to test mean wind speed homogeneity, if the observation data from meteorological stations are correct and intact, the direct test should be used firstly and then other methods can be used additionally.