Electric field soundings and the charge structure within an isolated thunderstorm

Electric field soundings and the charge structure within an isolated thunderstorm
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孤立雷暴内的电场探测和电荷结构

DOI:
10.1007/s11434-009-0471-1
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发表时间:
2010-03
期刊:
科学通报(英文版)
影响因子:
--
通讯作者:
She Yong
She Yong
中科院分区:
其他
文献类型:
--
作者:
Wang Huaibin;Qie Xiushu;Zhao zhongkuo;Sun Baolai;Zhang Hongfa;Zhang Tong;Wang Yong;Zhang Tinglong;She Yong

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设计了一套强电场探测系统,利用探测路径上的电场垂直分量、温度、相对湿度和沿着GPS资料,于2008年夏季在X波段天气雷达的配合下,对甘肃平凉地区雷暴内部的电场进行了现场观测。成功地获得了一个雷暴内部的电场分布。探测数据表明,沿探测轨迹有四个电荷层,沿着,三个在雷暴内部,一个在雷暴的下边界。低云边界电荷层是负的,作为一个屏蔽层,并奠定了4.3至4.5公里的ASL之间。下层正电荷中心(LPCC)位于4.5-5.3 km ASL(3°C至−2°C)之间;主要负电荷区位于5.4-6.6 km ASL(−3°C至−10°C)之间;上层正电荷层位于6.7-7.2 km ASL(−11°C至−14°C)之间。结果支持雷暴(0°C以上等温高度)内部的三极电荷结构,但中国内陆高原的LPCC比通常大得多。
A strong electric (E) field sounding system was designed to measure the vertical component of the E-fields, temperature, relative humidity and GPS data along the sounding path. In the summer of 2008,in situmeasurements of E-field inside the thunderstorms were conducted in Pingliang, Gansu Provience, with the cooperation of anX-band weather radar. One E-field profile inside a thunderstorm was successfully acquired. The sounding data indicated four charge layers along the sounding trajectory, three inside the thuderstorm and one at its lower boundary. The lower cloud boundary charge layer was negative, acting as a screening layer, and laid between 4.3 to 4.5 km ASL. The lower positive charge center (LPCC) existed between 4.5–5.3 km ASL (from 3°C to −2°C); the main negative charge area was present between 5.4–6.6 km ASL (−3°C to −10°C); the upper positive charge layer was between 6.7–7.2 km ASL (−11°C to −14°C). The results supports the tripole charge structure inside thunderstorms (above 0°C isotherm altitude), but the LPCC is much larger-than-usual in Chinese inland plateau.
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