Glaciation Flashcards
Define mass balance
Difference between inputs (accumulation) and outputs (ablation)
Determines if a glacier grows or shrinks
Define the zone of accumulation
Colder higher altitude areas with a positive mass balance (inputs > outputs) where the glacier advances
Define the zone of ablation
Warmer lower altitude areas with a negative mass balance where the glacier retreats
How does glacial ice form?
New snowflakes fall and compact pre-existing snow.
In summer meltwater percolates into the firn and refreezes to become dense. (Forms seasonal layers with darker stripes)
Over years this repeats and all air is squeezed out of snow forming glacial ice
Changes in mass balance over a year
Late autumn to early spring, glacier has a positive mass balance due to cooler temperatures so the glacier advances.
The most rapid accumulation is in winter.
Late spring and early autumn, glacier has a negative mass balance due to warmer temperatures so the glacier retreats.
The most rapid ablation is in summer.
Inputs causing accumulation
Precipitation
De-sublimation
Rock debris
Wind blown snow
Avalanche debris
Solar energy
Outputs causing ablation
Meltwater
Sublimation
Calving
Rock debris
Wind blown snow