| Project/Area Number |
05558051
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| Research Category |
Grant-in-Aid for Developmental Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Research Field |
Natural disaster science
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| Research Institution | KYUSHU UNIVERSITY |
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Principal Investigator |
TAKAHASHI Tsutomu KYUSHU UNIVERSITY,FACULTY OF SCIENCE,PROFESSOR, 理学部, 教授 (20197742)
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| Project Period (FY) |
1993 – 1995
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| Project Status |
Completed (Fiscal Year 1995)
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| Budget Amount *help |
¥7,000,000 (Direct Cost: ¥7,000,000)
Fiscal Year 1995: ¥800,000 (Direct Cost: ¥800,000)
Fiscal Year 1994: ¥3,400,000 (Direct Cost: ¥3,400,000)
Fiscal Year 1993: ¥2,800,000 (Direct Cost: ¥2,800,000)
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| Keywords | Cloud Particle Videosonde / Precipitation Mechanism / MCTEX Project / 雲粒子ビデオゾンデ / Hector / 雷活動 / MCTEX国際プロジェクト / 雲粒子 / 降水粒子ビデオゾンデ / 雷 / ビデオゾンデ / 降水機構 / 氷晶 / 集中豪雨 |
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| Research Abstract |
Whole knowledge of precipitation particle distribution in cloud in the prerequisite to increase our understanding of precipitation mechanisms of torrential rain producing clouds. Two types of videosonde systems were developed. One type aims to measure precipitation particles larger than 500mum in diameter. When precipitation particle interrupts the infra-red light running across the sight of camera, flash is triggered. The images are pictured by videocamera and sent to the ground by 1680 MHz. This videosonde system is also able to monitor both electric charge of precipitation particles, and temperature, humidity and pressure.
The other type of videosonde, cloud particle videosonde measures cloud droplets. The unique feature of this system is to take a picture of cloud particles on the film as it runs. Flash is used to make stational images of cloud droplets. Both videosonde systems were launched during the MCTEX project which was conducted at Melville Is., Australia. This was the first to elucidate the precipitation particles in the Hector clouds. Videosonde observation showed many frozen particles as large as 7 mm in diameter and abundant ice crystals, sometimes reaching to ten per cm^3. Analysis shows the very active ice phase process which may explain the most frequent lightning frequencies.
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