中山大学学报(自然科学版)
中山大學學報(自然科學版)
중산대학학보(자연과학판)
ACTA SCIENTIARUM NATURALIUM UNIVERSITATIS SUNYATSENI
2013年
5期
153-160,168
,共9页
刘智勇%周平%彭资%甘先华%郭乐东%赖仁审
劉智勇%週平%彭資%甘先華%郭樂東%賴仁審
류지용%주평%팽자%감선화%곽악동%뢰인심
标准化降水指数%Mann-Kendall趋势检验%旋转经验正交函数法%小波分析%广东省
標準化降水指數%Mann-Kendall趨勢檢驗%鏇轉經驗正交函數法%小波分析%廣東省
표준화강수지수%Mann-Kendall추세검험%선전경험정교함수법%소파분석%광동성
SPI%Mann-Kendall trend test%REOF%wavelet analysis%Guangdong Province
基于1960-2011年广东省25个地面气象站点的逐日气象资料,采用6个月尺度的标准化降水指数(SPI)为干旱评价指标,计算了广东省各站点每月的干旱指数,并在此基础上利用Mann-Kendall 趋势检验法、旋转经验正交函数法(REOF)、小波分析等方法分析了该地区干湿状况的时间演变趋势和空间分布特征。结果表明:广东省变干趋势的月份主要集中在1-3月,而变湿的月份主要为7-9月,且中部地区变湿趋势的月份数要明显多于东西部。此外,雨季(4-9月)广东东部及沿海大部分地区呈变湿趋势,而冬季全省大部分地区都表现为变干的趋势;根据REOF方法可将广东省干旱分布特征划分为4个典型的空间异常型:南岭型、粤西型、粤东型和雷州半岛型;各空间型对应的旋转主成分(PRC )序列分析结果表明,雨季各空间型都表现为统一的先变湿后变干趋势,而冬季除了雷州半岛型外则都表现为明显的变干趋势。小波分析结果表明各空间型干湿状况普遍存在1.5a、2~3a的显著变化周期。
基于1960-2011年廣東省25箇地麵氣象站點的逐日氣象資料,採用6箇月呎度的標準化降水指數(SPI)為榦旱評價指標,計算瞭廣東省各站點每月的榦旱指數,併在此基礎上利用Mann-Kendall 趨勢檢驗法、鏇轉經驗正交函數法(REOF)、小波分析等方法分析瞭該地區榦濕狀況的時間縯變趨勢和空間分佈特徵。結果錶明:廣東省變榦趨勢的月份主要集中在1-3月,而變濕的月份主要為7-9月,且中部地區變濕趨勢的月份數要明顯多于東西部。此外,雨季(4-9月)廣東東部及沿海大部分地區呈變濕趨勢,而鼕季全省大部分地區都錶現為變榦的趨勢;根據REOF方法可將廣東省榦旱分佈特徵劃分為4箇典型的空間異常型:南嶺型、粵西型、粵東型和雷州半島型;各空間型對應的鏇轉主成分(PRC )序列分析結果錶明,雨季各空間型都錶現為統一的先變濕後變榦趨勢,而鼕季除瞭雷州半島型外則都錶現為明顯的變榦趨勢。小波分析結果錶明各空間型榦濕狀況普遍存在1.5a、2~3a的顯著變化週期。
기우1960-2011년광동성25개지면기상참점적축일기상자료,채용6개월척도적표준화강수지수(SPI)위간한평개지표,계산료광동성각참점매월적간한지수,병재차기출상이용Mann-Kendall 추세검험법、선전경험정교함수법(REOF)、소파분석등방법분석료해지구간습상황적시간연변추세화공간분포특정。결과표명:광동성변간추세적월빈주요집중재1-3월,이변습적월빈주요위7-9월,차중부지구변습추세적월빈수요명현다우동서부。차외,우계(4-9월)엄동동부급연해대부분지구정변습추세,이동계전성대부분지구도표현위변간적추세;근거REOF방법가장광동성간한분포특정화분위4개전형적공간이상형:남령형、월서형、월동형화뇌주반도형;각공간형대응적선전주성분(PRC )서렬분석결과표명,우계각공간형도표현위통일적선변습후변간추세,이동계제료뇌주반도형외칙도표현위명현적변간추세。소파분석결과표명각공간형간습상황보편존재1.5a、2~3a적현저변화주기。
The monthly dryness/wetness conditions were calculated by applying the Standardized Precipi-tation index (SPI)at the 6 month scale based on the daily precipitation records of 25 meteorological sta-tions in Guangdong Province from 1960 to 2011.The methods including Mann-Kendall trend test,Rota-ted Empirical Orthogonal Function (REOF)and wavelet analysis were employed to detect the spatial and temporal patterns of dryness/wetness conditions over Guangdong Province.The results indicate:decrea-sing trends of SPI are identified mainly in January,February and March,while increasing trends are dominantly concentrated in July,August and September.In the middle part of the study area,the num-ber of months with increasing trends is more than in eastern and western parts.In addition,the eastern and coastal regions of Guangdong are characterized by increasing trends (wet tendency)of SPI in the rainy season (April to September),and the majority portion of Guangdong shows decreasing trends (dry tendency)of SPI in winter.According to the results of REOF,there are four main anomaly sub modes in Guangdong,i.e.,the Nanling,Leizhou Peninsula,the East and West Guangdong.All corresponding ro-tated principal components (RPC)of REOF indicate a wet-dry tendency in the rainy season,and all of them show a dry tendency in winter except the West Guangdong sub mode.1.5-year and 2 to 3-year peri-ods (significant atα=0.05 confidence level)can be investigated in all sub modes with the help of wave-let analysis.