Climatological characteristics and local influences on occurrence of freezing precipitation in Japan

Overview of attention for article published in Journal of the Japanese Society of Snow and Ice, January 2004

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降水過程（こうすいかてい、precipitation process）とは、空気中の水蒸気から雲が生成され水滴や氷晶が成長、降水である雨や雪などの形で降るまでのメカニズムのこと.

凍雨（とうう、）は、主に球形の透明な氷の粒が降る気象現象. 雨粒や解けかけの雪が落下の途中で再び凍ったもの.

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