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(Article of book - 1983)

Document title

Ablacja lodowcow sp ywajacych do morza, kszta towanie sie klifu lodowcowego i bariery lodowej oraz wynikajace stad implikacje dla bilansu masy lodowcow. in Polskie badania polarne 1970-1982.. (The ablation of glaciers flowing down to the sea, the formation of the ice cliff and ice front and the ensuing implications for the mass budget of the glaciers)

Authors(s) and Affiliation(s)

MARSZ A. A. ;

Abstract

The A. lists and systematizes the marine factors affecting the ablation of glaciers ending in the sea| they are different and supplementary in relation to those forming the course and size of ablation of glaciers ending on land. Using mathematical formulae, the rate of thermal abrasion on the ice-water border has been determined (using selected constant situational assumptions). The range length of the glacier into the sea has been established to the lines: a) of reaching isostatic balance, which e.g. at a snout thickness of 100 m and an inclination of the bedrock of 1 is 5.156 m. but at an inclination of bedrock of 6 and the same thickness it decreases to 856 m., and b) of cross-section of the glacier's surface with the water surface (theoretical situation). (L'A.).

Source

Book

Editor : Uniwerzytet Miko aja Kopernika, Torun - POLOGNE (1983)

Millesime : 1983 [pp. 209-223]

Bibliographic references : 4 réf.

Language

Polonais

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