CAJ | 학술논문

利用常州基本观测站1952-2007年长序列的雷暴观测资料和多普勒雷达回波资料,采用数理统计和小波变换方法,对常州雷暴的变化规律、周期特征以及雷达回波特征进行了分析.结果表明:(1)雷暴日数年代际间差异显著.(2)雷暴年际变化很大,最大值为最小值的5.9倍;雷暴日数总体呈显著减少的趋势.(3)夏季为雷暴高发季节,占总雷暴日数的66.8%.(4)月际变化差异大,雷暴集中出现在4-9月,其中7、8月为雷暴高发月.(5)从日分布来看,傍晚出现次数最多,其次为下午,上午出现最少.(6)常州年雷暴日数分布主要表现为12a(年代际)震荡周期贯穿在整个56年里;1952-2004年存在着非常明显7a左右的次周期特征;1968-2007年还存在3～4a的小周期特征.(7)常州雷暴的雷达回波基本反射率因子一般在30～65dBz之间,回波顶高为6～17km.(9)常州雷暴雷达回波移向主要有五类:西南东北向、东南西北向、西北东南向、旋转、局地生成.另外对常州雷雨大风和冰雹进行了统计分析,发现:7月为雷雨大风最高发月;5月和7月为冰雹最高发月.
이용상주기본관측참1952-2007년장서렬적뇌폭관측자료화다보륵뢰체회파자료,채용수리통계화소파변환방법,대상주뇌폭적변화규률、주기특정이급뢰체회파특정진행료분석.결과표명:(1)뇌폭일수년대제간차이현저.(2)뇌폭년제변화흔대,최대치위최소치적5.9배;뇌폭일수총체정현저감소적추세.(3)하계위뇌폭고발계절,점총뇌폭일수적66.8%.(4)월제변화차이대,뇌폭집중출현재4-9월,기중7、8월위뇌폭고발월.(5)종일분포래간,방만출현차수최다,기차위하오,상오출현최소.(6)상주년뇌폭일수분포주요표현위12a(년대제)진탕주기관천재정개56년리;1952-2004년존재착비상명현7a좌우적차주기특정;1968-2007년환존재3～4a적소주기특정.(7)상주뇌폭적뢰체회파기본반사솔인자일반재30～65dBz지간,회파정고위6～17km.(9)상주뇌폭뢰체회파이향주요유오류:서남동북향、동남서북향、서북동남향、선전、국지생성.령외대상주뇌우대풍화빙박진행료통계분석,발현:7월위뇌우대풍최고발월;5월화7월위빙박최고발월.
By using the long series observational data of thunderstorms in Changzhou from 1952 to 2007 and Doppler radar data,the variation,periodic chamcteristics and echo characters of thunderstorrns are studied by means of mathematical statistics and the wavelet analysis.The results show that the interdecadal thunderstorm variability is great,and the annual number of thunderstorm day has a decreasing trend.The interannual variation in thunderstorm day number is comparatively large with the maximum being 5.9 times the minimum.The obvious seasonal variation of thunderstorms can also be detected, and the period of April to September is more frequent months for thunderstorms and their occurrence in July and August is the most, and over 66.8% thunderstorms occur in summer season. From the diurnal distribution, the highest number is in the evening, followed by the afternoon, at least in the morning. The results from wavelet analysis show that the annual number of thunderstorm days in Changzhou has a period of about 12 years within nearly 56 years and there is a period of about 7 years from 1952 to 2004. In addition, there is still three to four years of small cycle characteristics from 1968 to 2007. It is found that the radar basic reflectivity of thunderstorms in Changzhou is from 30 to 65dBz and the echo top-high is between 6 to 17km and the thunderstorm radar echoes are in five major shifts: the southwest to northeast, the southeast to northwest, the northwest to southeast, the rotation, and the local generation. The strong wind and hail storm in Changzhou are analyzed using statistical analysis methods. It is found that the thunderstorm winds occurring in July rank on top and the hail occurs the most in May and July.