A study on lightning discharge precursor by taking advantages of simple structure and observation easiness of Tibetan thunderstorms
| Project/Area Number |
17404003
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 海外学術 |
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| Research Field |
Natural disaster science
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| Research Institution | Gifu University |
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Principal Investigator |
WANG Daohong Gifu University, Faculty of Engineering, Human Information and Systems Engineering, Associate Professor, 工学部, 助教授 (20273120)
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| Co-Investigator(Kenkyū-buntansha) |
TAKAGI Nobuyuki Gifu University, Faculty of Engineering, Electric and Electrical Engineering, Professor, 工学部, 教授 (80179415)
WATANABE Teiji Gifu University, Faculty of Engineering, Electric and Electrical Engineering, Professor, 工学部, 教授 (20021595)
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| Project Period (FY) |
2005 – 2006
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| Project Status |
Completed (Fiscal Year 2006)
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| Budget Amount *help |
¥6,700,000 (Direct Cost: ¥6,700,000)
Fiscal Year 2006: ¥3,100,000 (Direct Cost: ¥3,100,000)
Fiscal Year 2005: ¥3,600,000 (Direct Cost: ¥3,600,000)
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| Keywords | Lightning / Forecast of lightning / Lightning precursor / Ground discharges / Thunderstorm electricity / 雷前兆現象 |
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| Research Abstract |
We have performed a lightning observation campaign in Lhasa city, Tibet plateau region of China in the summers of 2005 and 2006. We found
1. Almost all Tibetan lightning occurred from late after noon to mid night. Thunderstorms differ greatly in lightning activity with some thunderstorms producing 20 flashes within one minute and some only a few even during their whole life period.
2. Many of the thunderstorms exhibit positive dominant electric fields at the ground and tend to produce smaller ratio of cloud-to-ground (CG) discharges. Among the CG discharges recorded, nearly 90% of them are negative ones. In general summer thunderstorms, the favorite condition for triggering a CG discharge may be the presence of the opposite polarity of pocket charge beneath a main charge region. For Tibeuan thunderstorms, a negative pocket charge may not exist just beneath the main positive charge which produced the dominant positive electric fields. This may account for the small number of CG discharges.
3. The lightning discharges are found to be initiated mainly at two heights : one is roughly 2 km and the other is 4 km above the ground. These results strongly suggest that the initial dominant leader of an intracloud discharge could be either a negative leader or a positive leader depending on its initial height. The large microsecond scale pulses usually observed at the initial stage of an intracloud discharge appeared to be generated when a negative leader is propagating within a positive charge region.
4. The CG ratio differs much during different stages of thunderstorms which suggest that favorite electrical charge structures for producing CG exist.
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Report
(3 results)
Research Products
(7 results)
