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Salju

Salju (dari bahaso Arab ثلج , salji, bahaso Inggirih: Snow) adolah bantuak padek aia nan jatuah ka bumi dari atmosfir atau awan nan alah mamboku manjadi kristal padek barupo es ketek dan ajak hujan nan manutupi sacaro parmanen atau samantaro (23 persen) dari saluruah parmukaan bumi. [1] Salju tadiri dari partikel uap aia kudian mandingin di udaro basobok angin dingin mahambui maluncua saroto pai manyublin (coliak atmosfir, biosfir, iklim, meteorologi, cuaco jatuah ka bumi sabagai kopiangan lunak, putiah, dan ajak kristal lunak kopiangan salju, pakih ajak kristal es, kalompok dari kasamuanyo). Daerah rawan salju utamo tamasuak daerah kutub, bagian paliang utaro dari bolahan bumi utaro dan daerah pagunungan di saluruah dunia dongan kalambaban nan cukuik dan suhu dingin. Di bolahan bumi salatan, salju turun tabateh tarutamo di daerah pagunuangan, salain Antartika.

Pangandapan

[suntiang | suntiang sumber]
  1. Media, Kompas Cyber. "Salju: Pengertian, Karakteristik, Proses, dan Manfaat". KOMPAS.com. Diakses tanggal 2020-12-30.
  • Media tantang Salju di Wikimedia Commons
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Salju
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