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Modification of raindrop size distribution due to seeder?feeder interactions between stratiform precipitation and shallow convection observed by X-band polarimetric radar and optical disdrometer
https://nied-repo.bosai.go.jp/records/2726
https://nied-repo.bosai.go.jp/records/27263e5d49b4-c958-483c-a1e4-ab52e938da0e
Item type | researchmap(1) | |||||||||||
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公開日 | 2023-03-30 | |||||||||||
タイトル | ||||||||||||
言語 | en | |||||||||||
タイトル | Modification of raindrop size distribution due to seeder?feeder interactions between stratiform precipitation and shallow convection observed by X-band polarimetric radar and optical disdrometer | |||||||||||
言語 | ||||||||||||
言語 | eng | |||||||||||
著者 |
Ryohei Misumi
× Ryohei Misumi
× Yasushi Uji
× Takeshi Maesaka
|
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抄録 | ||||||||||||
内容記述タイプ | Other | |||||||||||
内容記述 | The seeder?feeder interactions (SFIs), where raindrops from upper clouds grow by accreting cloud droplets in the lower clouds, have been extensively studied. However, there are few studies on the modification of raindrop size distribution (DSD) through this process. In the present study, rainfall from the landfalling rainbands of a typhoon was observed using an optical disdrometer and an X-band polarimetric radar. Rainfall was classified into the following three types based on the DSD characteristics at the surface and the existence of a ρ minimum in the upper layer: convective rainfall accompanied by a melting layer (type SF), convective rainfall without a melting layer (type C), and stratiform rainfall with a melting layer (type S). Type SF rainfall was regarded as having undergone SFIs between stratiform precipitation and shallow convection. The DSD for SF type rainfall was characterized by more small- to medium-sized raindrops and a larger normalized intercept parameter than rainfall types C and S. An analysis using vertical profiles of radar-derived DSD parameters for type SF rainfall suggested that the median-volume diameter of raindrops increased by accreting cloud droplets in the lower clouds, and that small- to medium-sized raindrops were produced by a warm rain process and breakup of raindrops. HV | |||||||||||
言語 | en | |||||||||||
書誌情報 |
en : Atmospheric Science Letters 巻 22, 号 7, 発行日 2021 |
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出版者 | ||||||||||||
言語 | en | |||||||||||
出版者 | WILEY | |||||||||||
ISSN | ||||||||||||
収録物識別子タイプ | EISSN | |||||||||||
収録物識別子 | 1530-261X | |||||||||||
DOI | ||||||||||||
関連識別子 | 10.1002/asl.1034 |