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- Imai I.
- Meteorological Research Institute
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- Fujiwara M.
- Meteorological Research Institute
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- Ichimura I.
- Meteorological Research Institute
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- Toyama Y.
- Meteorological Research Institute
書誌事項
- 公開日
- 1955
- DOI
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- 10.2467/mripapers1950.6.2_130
- 公開者
- Japan Meteorological Agency
この論文をさがす
説明
To investigate the radar reflectivity of falling snow, a continuous observation of size distributions of snow particles was made The fall velocity in relation to the melted diameter of snowflakes was studied simultaneously. The results show that a definite relationship between the radar reflectivity Z and the intensity of snowfall R exists for a duration of an hour or so. With the change in the degree of aggregation of snowflakes, an abrupt change of the coefficient occurs. The coefficients are some 3 to 10 times as great as that in MARSHALL'S relation. A brief discussion of the observed size-distribution curves is made.
収録刊行物
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- Papers in Meteorology and Geophysics
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Papers in Meteorology and Geophysics 6 (2), 130-139, 1955
Japan Meteorological Agency
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詳細情報 詳細情報について
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- CRID
- 1390282680425324288
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- NII論文ID
- 130004647954
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- ISSN
- 0031126X
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
- OpenAIRE
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- 抄録ライセンスフラグ
- 使用不可

