机构地区:[1]University of Science and Technology of China, School of Earth and Space Science [2]Key Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO), Institute of Atmospheric Physics, Chinese Academy of Sciences [3]Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology [4]State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences [5]State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences [6]Wuhan NARI Limited Liability Company, State Grid Electric Power Research Institute [7]Department of Physics, National Cheng Kung University [8]Department of Space Physics, School of Electronic Information, Wuhan University
出 处:《Earth and Planetary Physics》2019年第2期111-125,共15页地球与行星物理(英文版)
基 金:supported by the National Key Basic Research and Development Program (2017YFC1501501);National Natural Science Foundation of China (41574179, 41875006);National Natural Science Foundation for Excellent Youth of China (41622501);"The Hundred Talents Program" of Chinese Academy of Sciences (2013068);supported by funding from the NOAA Office of Global Programs for the Global Precipitation Climatology Project (GPCP);by NASA via the Tropical Rainfall Measuring Mission (TRMM);supported by NASA's HQ Earth S cience Data Systems (ESDS) Program
摘 要:The triangulation of red sprites was obtained, based on concurrent observations over a mesoscale convective system(MCS) in North China from two stations separated by about 450 km. In addition, broadband sferics from the sprite-producing lightning were measured at five ground stations, making it possible to locate and identify the individual causative lightning discharges for different elements in this dancing sprite event. The results of our analyses indicate that the sprites were produced above the trailing stratiform region of the MCS, and their parent strokes were located mainly in the peripheral area of the stratiform. The lateral offset between sprites and causative strokes ranges from a few km to more than 50 km. In a particularly bright sprite, with a distinct halo feature and streamers descending down to an altitude of approximately 48 km, the sprite current signal identified in the electric sferic, measured at a range of about 1,110 km, peaked at approximately 1 ms after the return stroke.The triangulation of red sprites was obtained, based on concurrent observations over a mesoscale convective system(MCS) in North China from two stations separated by about 450 km. In addition, broadband sferics from the sprite-producing lightning were measured at five ground stations, making it possible to locate and identify the individual causative lightning discharges for different elements in this dancing sprite event. The results of our analyses indicate that the sprites were produced above the trailing stratiform region of the MCS, and their parent strokes were located mainly in the peripheral area of the stratiform. The lateral offset between sprites and causative strokes ranges from a few km to more than 50 km. In a particularly bright sprite, with a distinct halo feature and streamers descending down to an altitude of approximately 48 km, the sprite current signal identified in the electric sferic, measured at a range of about 1,110 km, peaked at approximately 1 ms after the return stroke.
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