{"title":"斯里兰卡闪电分布的时空变异","authors":"U. Maduranga, M. Edirisinghe, L. Gamage","doi":"10.18052/WWW.SCIPRESS.COM/ILCPA.82.1","DOIUrl":null,"url":null,"abstract":"The variation of the lightning activities over Sri Lanka and surrounded costal belt (5.750N-10.000N and 79.50E-89.000E) is studied using lightning flash data of Lightning Imaging Sensor (LIS) which was launched in November 1997 for NASA’s Tropical Rainfall Measuring Mission (TRMM). The LIS data for the period of 1998 to 2014 are considered for this study. The spatial and temporal variation of lightning activities is investigated and respective results are presented. The diurnal variation over the studied area presents that maximum and minimum flash count recorded at 1530-1630 Local Time (10-11UTC) and 0530-0630LT (00-01UTC) respectively. Maximum lightning activities over the observed area have occurred after the 1330LT (08UTC) in every year during the considered time period. The seasonal variation of the lightning activities shows that the maximum lightning activities happened in First inter monsoon season (March to April) with 30.90% total lightning flashes and minimum lightning activities recorded in Northeast monsoon season (December to February) with 8.51% of total lightning flashes. Maximum flash density of 14.37fl km-2year-1 was observed at 6.980N/80.160E in First inter monsoon season. These seasonal lighting activities are agree with seasonal convective activities and temperature variation base on propagation of Intra-Tropical Convection Zone over the studied particular area. Mean monthly flash count presents a maximum in the month of April with 29.12% of lightning flashes. Variation pattern of number of lightning activities in month of April shows a tiny increment during the time period of 1998 to 2014. Maximum annual flash density of 28.09fl km-2yr-1 was observed at 6.980N/80.170E. The latitudinal variation of the lightning flash density is depicted that extreme lightning activities have happened at the southern part of the county and results show that there is a noticeable lack of lightning activities over the surrounded costal belt relatively landmass.","PeriodicalId":14453,"journal":{"name":"International Letters of Chemistry, Physics and Astronomy","volume":"139 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2019-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"8","resultStr":"{\"title\":\"Spatiotemporal Variability of Lightning Flash Distribution over Sri Lanka\",\"authors\":\"U. Maduranga, M. Edirisinghe, L. 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The seasonal variation of the lightning activities shows that the maximum lightning activities happened in First inter monsoon season (March to April) with 30.90% total lightning flashes and minimum lightning activities recorded in Northeast monsoon season (December to February) with 8.51% of total lightning flashes. Maximum flash density of 14.37fl km-2year-1 was observed at 6.980N/80.160E in First inter monsoon season. These seasonal lighting activities are agree with seasonal convective activities and temperature variation base on propagation of Intra-Tropical Convection Zone over the studied particular area. Mean monthly flash count presents a maximum in the month of April with 29.12% of lightning flashes. Variation pattern of number of lightning activities in month of April shows a tiny increment during the time period of 1998 to 2014. Maximum annual flash density of 28.09fl km-2yr-1 was observed at 6.980N/80.170E. 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引用次数: 8
摘要
利用美国国家航空航天局(NASA)热带雨量测量任务(TRMM)于1997年11月发射的闪电成像传感器(LIS)的闪电数据,研究了斯里兰卡及其周边沿海地带(5.750N-10.000N和79.50E-89.000E)的闪电活动变化。本研究考虑的是1998年至2014年期间的LIS数据。研究了雷电活动的时空变化规律,并给出了相应的结果。研究区闪数的日变化特征表明,闪数最大值和最小值分别出现在当地时间1530-1630 (10-11UTC)和0530-0630LT (00-01UTC)。在所考虑的时间段内,观测区域的最大闪电活动发生在每年1330LT (08UTC)之后。闪电活动的季节变化表明,第一季候风季(3 ~ 4月)的闪电活动最多,占总闪电的30.90%;东北季候风季(12 ~ 2月)的闪电活动最少,占总闪电的8.51%。第一季季风间期在6.98 n /80.160E观测到最大闪蒸密度为14.37fl km-2 -1。这些季节性光照活动与基于热带内对流带传播的季节性对流活动和温度变化一致。月平均闪电数在4月份最大,为29.12%。1998 - 2014年4月闪电活动次数的变化格局呈现出微弱的增加趋势。在6.98 n /80.170E,年闪蒸密度最大,为28.09fl km-2 year -1。闪电密度的纬向变化表明,县域南部发生了极端闪电活动,而周边沿海带相对陆块的闪电活动明显缺乏。
Spatiotemporal Variability of Lightning Flash Distribution over Sri Lanka
The variation of the lightning activities over Sri Lanka and surrounded costal belt (5.750N-10.000N and 79.50E-89.000E) is studied using lightning flash data of Lightning Imaging Sensor (LIS) which was launched in November 1997 for NASA’s Tropical Rainfall Measuring Mission (TRMM). The LIS data for the period of 1998 to 2014 are considered for this study. The spatial and temporal variation of lightning activities is investigated and respective results are presented. The diurnal variation over the studied area presents that maximum and minimum flash count recorded at 1530-1630 Local Time (10-11UTC) and 0530-0630LT (00-01UTC) respectively. Maximum lightning activities over the observed area have occurred after the 1330LT (08UTC) in every year during the considered time period. The seasonal variation of the lightning activities shows that the maximum lightning activities happened in First inter monsoon season (March to April) with 30.90% total lightning flashes and minimum lightning activities recorded in Northeast monsoon season (December to February) with 8.51% of total lightning flashes. Maximum flash density of 14.37fl km-2year-1 was observed at 6.980N/80.160E in First inter monsoon season. These seasonal lighting activities are agree with seasonal convective activities and temperature variation base on propagation of Intra-Tropical Convection Zone over the studied particular area. Mean monthly flash count presents a maximum in the month of April with 29.12% of lightning flashes. Variation pattern of number of lightning activities in month of April shows a tiny increment during the time period of 1998 to 2014. Maximum annual flash density of 28.09fl km-2yr-1 was observed at 6.980N/80.170E. The latitudinal variation of the lightning flash density is depicted that extreme lightning activities have happened at the southern part of the county and results show that there is a noticeable lack of lightning activities over the surrounded costal belt relatively landmass.