Multi-Parameter Radar Observation on the Formation Mechanism of Solid Precipitation Particles in a Broad Cloud Band Developed over the Sea of Japan in Winter
| Project/Area Number |
20740271
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| Research Category |
Grant-in-Aid for Young Scientists (B)
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| Allocation Type | Single-year Grants |
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| Research Field |
Meteorology/Physical oceanography/Hydrology
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| Research Institution | Nagoya University |
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Principal Investigator |
OHIGASHI Tadayasu Nagoya University, 地球水循環研究センター, 特任助教 (80464155)
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| Project Period (FY) |
2008 – 2009
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| Project Status |
Completed (Fiscal Year 2009)
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| Budget Amount *help |
¥4,420,000 (Direct Cost: ¥3,400,000、Indirect Cost: ¥1,020,000)
Fiscal Year 2009: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2008: ¥3,770,000 (Direct Cost: ¥2,900,000、Indirect Cost: ¥870,000)
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| Keywords | 固体降水 / マルチパラメーターレーダー / 偏波レーダー / 日本海 / 帯状降雪雲 / 豪雪・大雪 / 粒子識別法 / 降雪雲 / 寒気吹き出し / 豪雪 / 雲物理 |
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| Research Abstract |
A broad cloud band developed over the Sea of Japan is one of the cloud systems causing active snowfall during cold air outbreaks. This cloud band concentrates precipitation and occasionally causes a heavy snowfall. In this study, we conducted an observation using multi-parameter (polarimetric-Doppler) radar. A method identifying a main hydrometeor category from the radar data was developed and occurrence frequency for each hydrometeor type was examined. Appling the method to the case for a cloud band occurring during the observation period, the graupel type accounted for 30 to 40% of the total precipitation time. The snow aggregates type, which was the primary one, was about 50% of the total time.
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Report
(3 results)
Research Products
(16 results)
