南京信息工程大学学报
南京信息工程大學學報
남경신식공정대학학보
JOURNAL OF NANJING UNIVERSITY OF INFORMATION SCIENCE & TECHNOLOGY
2014年
5期
469-475
,共7页
袁飞%耿雪莹%孙明辉%周涛%关昊%高宇俊
袁飛%耿雪瑩%孫明輝%週濤%關昊%高宇俊
원비%경설형%손명휘%주도%관호%고우준
雷暴%气候特征%区划%小波分析%信息扩散
雷暴%氣候特徵%區劃%小波分析%信息擴散
뇌폭%기후특정%구화%소파분석%신식확산
thunderstorm%climatic characteristics%regionalization%wavelets analysis%information diffusion
利用廊坊市9个气象站1964-2011年的雷暴日资料,通过数理统计、线性趋势拟合和小波分析,研究了廊坊市近48 a来雷暴的时空分布特征和周期性特征,并结合信息扩散法,进行了不同雷暴日数下的概率区划。结果表明:廊坊市雷暴日的年际变化幅度较大,年均雷暴日数总体呈下降趋势,约每10 a减少2 d;廊坊市雷暴月、季变化呈明显的单峰型,雷暴主要发生在4-10月,其中夏季(6-8月)占全年的74?5%;中北部的雷暴日数明显多于南部地区;10 a及以上周期在绝大部分地区具有全域性,而短周期3~5 a大多表现在20世纪90年代之前;随着雷暴日数的增大,雷暴发生高概率区逐渐北移,当雷暴日数异常偏大(>40 d)时,中部的部分地区也处于雷暴发生高概率区。
利用廊坊市9箇氣象站1964-2011年的雷暴日資料,通過數理統計、線性趨勢擬閤和小波分析,研究瞭廊坊市近48 a來雷暴的時空分佈特徵和週期性特徵,併結閤信息擴散法,進行瞭不同雷暴日數下的概率區劃。結果錶明:廊坊市雷暴日的年際變化幅度較大,年均雷暴日數總體呈下降趨勢,約每10 a減少2 d;廊坊市雷暴月、季變化呈明顯的單峰型,雷暴主要髮生在4-10月,其中夏季(6-8月)佔全年的74?5%;中北部的雷暴日數明顯多于南部地區;10 a及以上週期在絕大部分地區具有全域性,而短週期3~5 a大多錶現在20世紀90年代之前;隨著雷暴日數的增大,雷暴髮生高概率區逐漸北移,噹雷暴日數異常偏大(>40 d)時,中部的部分地區也處于雷暴髮生高概率區。
이용랑방시9개기상참1964-2011년적뇌폭일자료,통과수리통계、선성추세의합화소파분석,연구료랑방시근48 a래뇌폭적시공분포특정화주기성특정,병결합신식확산법,진행료불동뇌폭일수하적개솔구화。결과표명:랑방시뇌폭일적년제변화폭도교대,년균뇌폭일수총체정하강추세,약매10 a감소2 d;랑방시뇌폭월、계변화정명현적단봉형,뇌폭주요발생재4-10월,기중하계(6-8월)점전년적74?5%;중북부적뇌폭일수명현다우남부지구;10 a급이상주기재절대부분지구구유전역성,이단주기3~5 a대다표현재20세기90년대지전;수착뇌폭일수적증대,뇌폭발생고개솔구축점북이,당뇌폭일수이상편대(>40 d)시,중부적부분지구야처우뇌폭발생고개솔구。
Using the data of thunderstorm days recorded by the 9 weather stations in Langfang of Hebei province from 1964 to 2011, the temporal-spatial distribution characteristics and periodicity features during the recent 48 years are analyzed by means of mathematical statistics,linear trend fittings and wavelets analysis.The regionalization of thunderstorm probability of different number of days is worked out by use of information diffusion theory.The re-sults show that the interannual thunderstorm variability is significant and the annual thunderstorm days has a decrea-sing trend.The numerical value of decreasing days is about 2d per decade. The seasonal variation exhibits a uni-peak-type and the thunderstorms mainly occur from April to October,while 74?5% of thunderstorms occur in the three-month of June,July and August during the summer. The thunderstorm days in north-central areas are signifi-cantly more than that in south.The variation periods are stable and exist across the whole region in most areas when they are more than 10a,but the short period of 3 to 5 years mainly happens before the 1990s. With the increase of the thunderstorm days,the high probability areas move north.Some of the central areas will be high probability areas when the thunderstorm days become abnormally high.