热带地理
熱帶地理
열대지리
TROPICAL GEOGRAPHY
2013年
6期
689-694
,共6页
朱传林%段振中%李国梁%柴健%贾沛%马虹旭
硃傳林%段振中%李國樑%柴健%賈沛%馬虹旭
주전림%단진중%리국량%시건%가패%마홍욱
大气环流%武当山%闪电%时空分布
大氣環流%武噹山%閃電%時空分佈
대기배류%무당산%섬전%시공분포
atmosphere circulation%the Wudangshan Mountains%lightning%spatial-temporal distribution
武当山是世界文化与自然遗产,因而武当山风景区的雷电防护尤为重要。截取风景区的地闪数据,以1 km2范围为基本单元,得到各单元内2008-01-01-2011-12-31期间的全部地闪频次、极性、强度等参数,分析武当山风景区雷电环境及武当山地理环境对雷电活动的影响。研究表明:研究区域闪电集中发生在6-8月份的午后T 14:00-18:00。闪电频数日变化规律明显,最大值出现在T 16:00,最小值出现在T 10:00-11:00。雷击大地密度整体上随高度表现出明显的增长趋势,雷电流强度平均值与高度大致呈现反向分布趋势,拟合出的雷击大地密度与高度关系式的相关系数R达0.83456。大气环流特征表明,武当山雷电天气主要有3种类型:副热带高压西北部雷电型、高空槽雷电型和低涡雷电型,其中副热带高压西北部雷电型占主导。
武噹山是世界文化與自然遺產,因而武噹山風景區的雷電防護尤為重要。截取風景區的地閃數據,以1 km2範圍為基本單元,得到各單元內2008-01-01-2011-12-31期間的全部地閃頻次、極性、彊度等參數,分析武噹山風景區雷電環境及武噹山地理環境對雷電活動的影響。研究錶明:研究區域閃電集中髮生在6-8月份的午後T 14:00-18:00。閃電頻數日變化規律明顯,最大值齣現在T 16:00,最小值齣現在T 10:00-11:00。雷擊大地密度整體上隨高度錶現齣明顯的增長趨勢,雷電流彊度平均值與高度大緻呈現反嚮分佈趨勢,擬閤齣的雷擊大地密度與高度關繫式的相關繫數R達0.83456。大氣環流特徵錶明,武噹山雷電天氣主要有3種類型:副熱帶高壓西北部雷電型、高空槽雷電型和低渦雷電型,其中副熱帶高壓西北部雷電型佔主導。
무당산시세계문화여자연유산,인이무당산풍경구적뇌전방호우위중요。절취풍경구적지섬수거,이1 km2범위위기본단원,득도각단원내2008-01-01-2011-12-31기간적전부지섬빈차、겁성、강도등삼수,분석무당산풍경구뇌전배경급무당산지리배경대뇌전활동적영향。연구표명:연구구역섬전집중발생재6-8월빈적오후T 14:00-18:00。섬전빈수일변화규률명현,최대치출현재T 16:00,최소치출현재T 10:00-11:00。뢰격대지밀도정체상수고도표현출명현적증장추세,뇌전류강도평균치여고도대치정현반향분포추세,의합출적뢰격대지밀도여고도관계식적상관계수R체0.83456。대기배류특정표명,무당산뇌전천기주요유3충류형:부열대고압서북부뇌전형、고공조뇌전형화저와뇌전형,기중부열대고압서북부뇌전형점주도。
Lightning prevention is particularly important for the Wudangshan Mountains Scenic Region, which has been listed as a site of World Cultural and Natural Heritage. With the range of 1 km2 (1 km ×1 km) being the basic unit, the lightning frequency, polarity, intensity and other parameters in each unit from Jan. 1st, 2008 to Dec. 31st, 2011 are gained for the whole region. At the same time, the influences of geological features and the lightning environment and geographical environment of the Wudangshan Mountains on lightning activities are analyzed. The results show that:most of the lightning happens at T14-18 in June-August. The daily variation of lightning frequency is obvious in each area, the peak appears at T16:00, while the minimum value at T10-11. The lightning frequency increases with the increase of altitude, while the average lightning current intensity decreases in the mountainous areas. As a result, the correlation coefficient between the lightning density and the elevation is 0.834 56. The atmospheric circulation characteristics indicate that there are three main types of lightning storms in the Wudangshan Mountains: there are subtropical high of the northwest lightning type,upper-level trough lightning type and vortex lightning type, in which the northwest lightning type of the subtropical high dominates the area.