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Wiktionary英語版での「graupel」の意味 |
graupel
出典:『Wiktionary』 (2025/04/19 20:28 UTC 版)
語源
Borrowed from German Graupel(wetter) (literally “graupel (weather)”). Graupel is a back-formation from graupeln (“to hail (with soft hailstones)”) + -el (diminutive suffix); and graupeln is from Graupe (“hulled grain, pearl barley”) (ultimately from Proto-Slavic *krūpà (“grainy substance; groats; hail”) and Proto-Indo-European *krewp-) + -eln (suffix forming verbs, often with a diminutive or frequentative sense).
発音
- (Received Pronunciation, General American) IPA: /ˈɡɹaʊp(ə)l/
- ハイフネーション: graup‧el
名詞
graupel (countable and uncountable, plural graupels) (meteorology)
- (uncountable) A precipitation that forms when supercooled droplets of water condense on a snowflake.
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1876 November 2, “Notes”, in Nature: A Weekly Illustrated Journal of Science, volume XV, London; New York, N.Y.: Macmillan and Co., →OCLC, page 17:
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In a paper in this month's Petermann's Mittheilungen Prof. H. Fritz treats of the Geographical Distribution of Hail. […] [B]alls of true hail hav[e] an icy structure, whereas the balls of graupel are only small pellets of snow. […] With increase in latitude and in height the fall of graupel increases and that of hail decreases, while hailstones of large size are most frequent towards the equator.
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- (countable) A small ball of rime resulting from this process.
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1951 September 15, Donald G. Yerg, “Tikhomirov, E., On the Shape of Graupels and Hailstones (O Forme Krupy i Grada). Meteorologiia i Gidrologiia, 2, No. 9: 66–67, 1936”, in Annotated Bibliography on Snow, Ice, and Permafrost […] (SIPRE Report; 12), [Hanover, N.H.]: Snow, Ice, and Permafrost Research Establishment, Corps of Engineers, United States Army, →ISSN, →OCLC, page 340, column 2:
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It is established that graupels and hailstones are cone-shaped with rounded apexes and that they become egg-shaped as a result of growth during descent.
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2013, Pao K[uan] Wang, “The Shape and Size of Cloud and Precipitation Particles”, in Physics and Dynamics of Clouds and Precipitation, Cambridge, Cambridgeshire: Cambridge University Press, →ISBN, page 30:
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[W]hen an ice or snow crystal collides with supercooled droplets, the droplets will freeze on the surface of the crystal to form rime. […] [C]ontinued riming will eventually produce a particle that is completely covered by rimes such that the original crystal shape can no longer be recognized. The particle now becomes a graupel (sometimes also called a soft hail or snow pellet). […] By convention, a graupel should be smaller than 5 mm in diameter. If it becomes greater than 5 mm in diameter (2.5 mm in radius) it will be called hail.
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参照
- ^ “graupel, n.”, in OED Online
, Oxford: Oxford University Press, December 2024.
- ^ “graupel, n.”, in Lexico, Dictionary.com; Oxford University Press, 2019–2022.
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Text is available under Creative Commons Attribution-ShareAlike (CC-BY-SA) and/or GNU Free Documentation License (GFDL). Weblio英和・和英辞典に掲載されている「Wiktionary英語版」の記事は、Wiktionaryのgraupel (改訂履歴)の記事を複製、再配布したものにあたり、Creative Commons Attribution-ShareAlike (CC-BY-SA)もしくはGNU Free Documentation Licenseというライセンスの下で提供されています。 |
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