Glacier ice accumulation
id:
glacier-ice-accumulation-254-7747733
title:
Glacier ice accumulation
text:
Glacier ice accumulation occurs through accumulation of snow and other frozen precipitation, as well as through other means including rime ice, avalanching from hanging glaciers on cliffs and mountainsides above, and re-freezing of glacier meltwater as superimposed ice. Accumulation is one element in the glacier mass balance formula, with ablation counteracting. With successive years in which accumulation exceeds ablation, then a glacier will experience positive mass balance, and its terminus wi
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Glacier_ice_accumulation
date created:
date modified:
2022-08-01T11:47:48Z
main entity:
{"identifier":"Q690578","url":"https://www.wikidata.org/entity/Q690578"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/5/5c/Hanging_glacier_chugach_nf.jpg","width":330,"height":512}
fields total:
13
integrity:
14