Lightning and Doppler radar observations of a squall line system
文献类型：期刊论文
| 作者 | Feng, Guili1,2; Qie, Xiushu3; Wang, Jun4; Gong, Dianli4 |
| 刊名 | ATMOSPHERIC RESEARCH
 |
| 出版日期 | 2009-02-01 |
| 卷号 | 91期号:2-4页码:466-478 |
| 关键词 | Lightning activity Radar observation Satellite Squall line Damaging wind |
| ISSN号 | 0169-8095 |
| DOI | 10.1016/j.atmosres.2008.05.015 |
| 通讯作者 | Feng, Guili(fenggl@lzb.ac.cn) |
| 英文摘要 | A typical squall line with damaging wind and hailstones occurred on 28 April 2006 in Shandong Province, middle eastern China, and caused great economic loss. The characteristics of cloud-to-ground lightning (CC) in the squall line were studied in detail by combining the data from the ground-based CC location network, two Doppler radars and the Lightning Imaging Sensor on the TRMM satellite. Results show that positive CC flashes accounted for 54.7% of the total CC flashes. During the initial developing stage, the CG flash rate was lower than 0.5fl min(-1) and most of the CC flashes were positive. It increased significantly, up to 4.5fl min(-1), along with the rapid development of the squall line, and the percentage of positive CG was more than 75% during this period. The CG flash rate began to decrease but the percentage of negative CC flash increased gradually and exceeded that of positive CC during the mature and dissipating stages. Positive CC flashes tended to occur on the right flank and negative ones on the left flank. Strong wind at the surface occurred in or near the regions with dense positive CC flashes. Almost all positive CG flashes occurred near the strong radar echo regions, in the front parts of the squall line. However, the negative CC flashes almost exclusively occurred in the regions with weak and uniform radar echoes. The total flash rate in the storm was very high, up to 136fl min(-1), and its ratio of intracloud flashes (IC) to CC flashes was 35:1. Dense positive CC flashes corresponded to updraft regions, they did not occur in the core of the updraft, but just behind and close to the main updraft instead. The rear inflow jet, between 3 and 6 km, played an important role in the formation of the bow echo and very strong wind at surface. The CC distribution features in the squall line were obviously different from that of an ordinary MCS. The charge structure could be roughly described as an inverted charge structure. (C) 2008 Elsevier B.V. All rights reserved. |
| 收录类别 | SCI ; ISTP |
| WOS关键词 | MESOSCALE CONVECTIVE SYSTEM ; CONTIGUOUS UNITED-STATES ; CHARGE STRUCTURE ; PRECIPITATION ; THUNDERSTORMS ; EVOLUTION ; POLARITY ; STORM ; SUPERCELL ; SATELLITE |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| WOS类目 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000263193900043 |
| 出版者 | ELSEVIER SCIENCE INC |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2556192 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Feng, Guili |
| 作者单位 | 1.Shandong Res Inst Meteorol, Jinan 250031, Shandong, Peoples R China 2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou, Gansu, Peoples R China 3.Chinese Acad Sci, Inst Atmospher Phys, Lab Middle Atmosphere & Global Environm Observat, Beijing, Peoples R China 4.Shandong Weather Modificat Off, Jinan, Shandong, Peoples R China |
| 推荐引用方式 GB/T 7714 | Feng, Guili,Qie, Xiushu,Wang, Jun,et al. Lightning and Doppler radar observations of a squall line system[J]. ATMOSPHERIC RESEARCH,2009,91(2-4):466-478. |
| APA | Feng, Guili,Qie, Xiushu,Wang, Jun,&Gong, Dianli.(2009).Lightning and Doppler radar observations of a squall line system.ATMOSPHERIC RESEARCH,91(2-4),466-478. |
| MLA | Feng, Guili,et al."Lightning and Doppler radar observations of a squall line system".ATMOSPHERIC RESEARCH 91.2-4(2009):466-478. |
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来源：寒区旱区环境与工程研究所
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