Lecture 3: Glacier hydrology Flashcards
The hydrological regimes of snow covered and glaciated catchments are similar in that, from December to March, groundwater discharge is equal to total discharge. What however, is the main way in which they differ?
Snow covered catchments do not have a glacial component of discharge, by which icemelt, firnmelt and snowmelt contribute a significant proportion of the discharge of glaciated catchments from June to October.
Water flow is governed by variations in hydraulic potential. How is this determined at the surface compared to subsurface?
Surface hydraulic potential governed by elevation.
Sub-surface determined by elevation and water pressure (from the size/shape of conduit and pressure and density of overlying ice).
Where are the supra-, En-, Pro- and Sub- glacial environments found on a glacier?
Supra = surface En = in Sub= beneath ice Pro = in front of ice
Name two features of the supraglacial environment.
Cryconite holes / ice carved streams
By what feature does water leave the supraglacial environment for the englacial?
Moulins
How does water flow into the proglacial environment?
Via release of subglacial water and throughflow of surface melt.
Describe the flow in proglacial environments.
Flows through unconfined material and braided, dynamic channels.
What is Bulk meltwater monitoring?
Annual/seasonal hydrograph or chemograph reveals drainage system.
Describe the use of hydrochemistry.
The chemical composition of bulk meltwaters used to infer chemical weathering environment and therefore the hydrological flow path.
Describe the 3 key features of dye-tracing.
- Known quantity of dye injected into moulin/crevasse
- Dye concentration monitored in BMW
- Hydrograph of water velocities plotted from dye return.
What would a return curve of fast velocities show about the hydrological system? What would double peaks show?
- fast return = pressure and free flow in main conduits.
- Double peaks = braided conduit.
Borehole investigations allow the subglacial drainage system to be measured directly, but how are they carried out?
- Boreholes drilled into glacier bed using hot water / steam drill.
- Sensors installed
- Borehole waters samples
- Dye traces conducted
When is it easiest to investigate ice caves and why is this a problem?
Easiest to measure after glacial lake outburst but very dangerous.
As expected, what is the pattern of variation in borehole water level though the glaciers depth?
Variation increase in frequency and magnitude towards the ice surface.
What can variations in subglacial water pressure lead to?
Till deformation