A Study of Cumulonimbus in Generating and Developing Stage Observed by Ka-Band Cloud Radar and Multi-sensor
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- NAKAKITA, Eiichi
- Disaster Prevention Research Institute, Kyoto University
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- NIIBO, Tomohiro
- Breau of Tohoku Region, KitakamiRiver Integrated DAM Management office, MLIT .
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- OHIGASHI, Tadayasu
- National Research Institute for Earth Science and Disaster Resilience
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- YAMAGUCHI, Kosei
- Disaster Prevention Research Institute, Kyoto University
Bibliographic Information
- Other Title
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- Kaバンド雲レーダー等のマルチセンサーで捉えた積乱雲の生成・発達過程
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Description
Suddenly-generated and rapidly-developed isolated cumulonimbus often cause flash flood and inundation disasters. For these disasters prediction, it is significant to analyze flow structure in a cumulonimbus cloud before raindrop generation. To investigate the initiation process, we conducted observation in Kobe City, on August 2018 using a Ka-band Doppler radar, X-band radars and some sensors. Developing cumulonimbus clouds and non-precipitating cumulus were observed by Ka-band radar, and the former has high Radar reflectivity (Zh) in the upper part. This implies that strong updraft lifted up the cloud particles and particle size grew up in the developing cell. In addition, we evaluated the effect of spatial resolution and direction on the radar observation by analyzing the vortex structure simulated by a Large Eddy Simulation model. The simulation result show that the vorticity can be observed irrespective of the direction if a cell has a circulation in a spatial scale larger than observation.
Journal
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- Disaster Prevention Research Institute Annuals. B
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Disaster Prevention Research Institute Annuals. B 62 (B), 399-431, 2019-09
京都大学防災研究所
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Details 詳細情報について
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- CRID
- 1050001338940132608
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- NII Article ID
- 120006770323
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- NII Book ID
- AN00027784
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- ISSN
- 0386412X
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- HANDLE
- 2433/244974
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- Text Lang
- ja
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- Article Type
- departmental bulletin paper
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- Data Source
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- IRDB
- CiNii Articles
- KAKEN