电网技术
電網技術
전망기술
POWER SYSTEM TECHNOLOGY
2013年
5期
1425-1431
,共7页
赵伟%童杭伟%张俊%浦静姣
趙偉%童杭偉%張俊%浦靜姣
조위%동항위%장준%포정교
雷暴日%地闪密度%地闪强度%相关分析%土地利用类型
雷暴日%地閃密度%地閃彊度%相關分析%土地利用類型
뇌폭일%지섬밀도%지섬강도%상관분석%토지이용류형
thunderstorm day%density of cloud-to-ground lightning%intensity of cloud-to-ground lightning%correlation analysis%land use type
根据浙江省建站始到2011年70个地面观测站的雷暴日资料、浙江省电力部门闪电定位系统的2005—2011年地闪数据和电网雷害资料,分析研究了浙江省雷电的时空分布特征及影响因素。研究结果表明:浙江省雷电主要集中在3—9月,多发生在15—16时段。全省雷暴日分布呈现山区比平原地区多,内陆比沿海多的特点。地闪密度呈现明显的地域性差异,地闪高密度区表现为两大片、若干点的分布。负闪占总地闪的百分率为94.91%。正、负闪电强度主要集中在0~50 kA。地闪高密度区的分布,与气候、地形、地貌、地面大型水体和城市热岛效应有着密切关系。
根據浙江省建站始到2011年70箇地麵觀測站的雷暴日資料、浙江省電力部門閃電定位繫統的2005—2011年地閃數據和電網雷害資料,分析研究瞭浙江省雷電的時空分佈特徵及影響因素。研究結果錶明:浙江省雷電主要集中在3—9月,多髮生在15—16時段。全省雷暴日分佈呈現山區比平原地區多,內陸比沿海多的特點。地閃密度呈現明顯的地域性差異,地閃高密度區錶現為兩大片、若榦點的分佈。負閃佔總地閃的百分率為94.91%。正、負閃電彊度主要集中在0~50 kA。地閃高密度區的分佈,與氣候、地形、地貌、地麵大型水體和城市熱島效應有著密切關繫。
근거절강성건참시도2011년70개지면관측참적뇌폭일자료、절강성전력부문섬전정위계통적2005—2011년지섬수거화전망뇌해자료,분석연구료절강성뇌전적시공분포특정급영향인소。연구결과표명:절강성뇌전주요집중재3—9월,다발생재15—16시단。전성뇌폭일분포정현산구비평원지구다,내륙비연해다적특점。지섬밀도정현명현적지역성차이,지섬고밀도구표현위량대편、약간점적분포。부섬점총지섬적백분솔위94.91%。정、부섬전강도주요집중재0~50 kA。지섬고밀도구적분포,여기후、지형、지모、지면대형수체화성시열도효응유착밀절관계。
Based on the recorded data of thunderstorm days from 70 surface observation stations in Zhejiang province ever since their building up to 2011 and the cloud-to-ground lightning data recorded by lightning detection and location system of Zhejiang power bureau and the record of damages caused by thunders from 2005 to 2011, the temporal-spatial distribution characteristics of thunder and lightning in Zhejiang province and influencing factors are analyzed and researched. Research results show that the lightning phenomena mainly appear from March to September and mostly happen in the time period from 15:00 to 16:00. The distribution of thunderstorm days present such a feature that the amount of thunderstorm days appear in mountain area is more than that in plain area, and that in inland area is more than that in coastal areas. There is obvious regional difference in the density distribution of cloud-to-ground lightning: it appears as the distribution in two large areas and several points. The percentage of negative cloud-to-ground lightning in total cloud-to-ground lightning is 94.91%. The positive and negative lightning intensities mainly appear in the range from 0 kA to 50 kA. The distribution of areas with high density of cloud-to-ground lightning in Zhejiang province is bound up with whether, landform, topographic feature, surface large-scale water mass and urban heat island effect.