Mass Balance, Transport and past glaciations Flashcards
Mass balance (b)
= accumulation (c) + ablation (a)
Mass balance (b) = accumulation (c) + ablation (a) Positive mass balance
More accumulation than melting
Glacier advance
Mass balance (b) = accumulation (c) + ablation (a) Negative mass balance
More ablation than accumulation
Glacier retreat
Measuring mass balance
Manual collection of mass balance
Accumulation zone
Pits (to check how much snow has fallen)
You can dig down into the glacier and see how much snow is deposited each year (quite easy to see)
Measuring mass balance
Manual collection of mass balance
Ablation zone
Stakes
You can dig down into the glacier and see how much snow is deposited each year (quite easy to see)
Positive mass balance measurements are very…
detailed
Negative mass balance measurements are very…
very slow and expensive, small scale
Positives of remote sensing
potentially cover large huge areas, could be semi automatic
Negatives of remote sensing
may be problems with technique on small glaciers
What is Global Land Ice Measurements from Space (GLIMS) used to do?
Using the World’s Glaciers to Monitor Climate Change
Glacial transport paths
Supraglacial
Englacial
Subglacial
Sediment sources
Supraglacial debris Subglacial debris - Regelation - Shearing - Freezing on
Pressure melting point
The pressure melting point is the temperature at which ice melts at a given pressure.
Positive mass balance
More accumulation than melting
Glacier advance
There is more accumulation than melting so glacier advance
Negative mass balance
More ablation than accumulation than accumulation
Glacier retreat
More ablation meaning the glacier retreats
The glacier is always moving forward (but it may retreat)
In the summer, the snow melts back at the front
In the higher part there is more accumulation (accumulation dominant)
The lower part is more ablation (called ablation dominant)