Nilas

Nilas
Nilas Meereis als Anfangsstadium von Frazil-Eis

Nilas ist eine dünne, elastische Eisschicht. Diese dünne Neueisdecke entsteht durch die Verdickung von Eis. Abhängig von der Dicke, wird zwischen dunklem Nilas (< 5 cm) und hellem Nilas (> 5 cm) unterschieden.

Siehe auch

Quellen

  • Frank Lindemann: Sedimente im arktischen Meereis - Eintrag, Charakterisierung und Quantifizierung. (Ber. Polarforsch. 283) 1998 (PDF).
  • Alfred-Wegener-Institut für Polar- und Meeresforschung: Meereis (PDF).

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