Śńyg: Zimowy ôpad atmosferyczny
Śńyg to je atmosferyczny uopad we postaći krysztołkůw lodu, nojczyńśći we formje szyśćoramjynnych gwjozdkůw.
Tworzům uůne na źymji śńyżno deka. Śnyg powstowo we wyńiku krystalizacyji pary wodnyj.
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