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Physical Process

Glacial Retreat

Glacial and Periglacial Processes

The net loss of a glacier's ice over time as melting and calving at its margin outpace the accumulation of new snow and ice further up its length, causing the glacier's front to migrate back up-valley. Sustained glacial retreat across most of the world's mountain glaciers over the past century is among the clearest visible signals of global warming.

Facts
Partially Attested
Timescale
Decades to centuries (documented retreat since 1850) 1
The source dates the well-documented retreat to the period since 1850 and gives no single characteristic timescale for the process itself.
Process Type
Glacial 1
Connections

Causes

Sources
1. Retreat of glaciers since 1850, Wikipedia
  • Causes section, mass balance paragraph
    If the accumulation is less than the ablation, the glacier will retreat.
  • Introduction, opening sentence
    The retreat of glaciers since 1850 is a well-documented effect of climate change.
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