Glacier Mass Balance Flashcards
Glaciers mass balance
Difference between the amount of snow/ice accumulation and the amount of ablation in 1 year
Accumulation zone
Glaciers gain mass in the accumulation zone (upper part of glacier where Input EXCEEDS output)
Ablation zone
Mass is lost in the ablation zone (lower part of glacier where output EXCEEDS input)
Equilibrium (with mass balance)
At the transition between the 2 zones, accumulation = ablation, this boundary is known as equilibrium. This decides the position of the snow line
Accumulation > ablation
When a glacier gains more mass than it looses then the
Mass balance = positive
This causes the snout of the glacier to advance
Accumulation < Ablation
If the mass balance is negative (looses more mass than the glacier gains) then the glaciers snout will retreat
Accumulation = ablation
If the glacier neither gains or looses mass, the balance is zero and the snout remains stationary
Factors that impact the mass balance
Climate change - demonstrated by the gradual and sustained release of all of the world’s glaciers over the past 150 years in response to global warming
Weather change - weather changing all year round effects the mass balance as it makes it not constant