Ablation of snow‐fields at high altitudes by radiant solar heat

Eos, Transactions, American Geophysical Union
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Abstract

Snowfields and the so‐called névés of glaciers on lofty mountains often present a peculiar, honeycombed appearance, the surface being pitted with deep cell‐like hollows a foot or two feet in diameter and from a few inches to several feet in depth. When typically developed these hollows are closely spaced, the divides between them consisting merely of attenuated blades and pinnacles of hard, granular snow (Fig. 1). The hollows are alined roughly in rows and sunk at a uniform, high angle, all in the same direction.

Publication type Article
Publication Subtype Journal Article
Title Ablation of snow‐fields at high altitudes by radiant solar heat
Series title Eos, Transactions, American Geophysical Union
DOI 10.1029/TR015i002p00380
Volume 15
Issue 2
Year Published 1934
Language English
Publisher American Geophysical Union
Description 6 p.
First page 380
Last page 385
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