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Accretion (meteorology) : ウィキペディア英語版 | Accretion (meteorology) Accretion is defined as the gradual collection of something over time.〔(Accretion (definition) ) Merriam-Webster. Retrieved 14 February 2014.〕 In meteorology it is the process of accumulation of frozen water as precipitation over time as it descends through the atmosphere. The collection of these particles eventually forms snow or hail in clouds and depending on lower atmosphere temperatures may become rain or sleet.〔(National Snow and Ice Data Center ). Retrieved 14 February 2014.〕 Accretion is the basis for cloud formation and can also be seen as water accumulates on the particulate matter and form jet contrails. This is because water vapor in the air requires condensation nuclei to form large droplets of solid or liquid water.〔(NOAA accretion ) NOAA. Retrieved 14 February 2014.〕 ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Accretion (meteorology)」の詳細全文を読む
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