Final - Snow Flashcards
What are 4 simultaneous estimation problems related to snow?
- the quantity of water held in snowpacks
- the magnitude and rate of water lost to the atmosphere by sublimation
- The timing, rate, and magnitude of snow melt
- The fate of melt water
What are the aims of the Canadian Cryospheric Information Network
- To provide a data and information management infrastructure for the Canadian cryospheric research community
- To enhance public awareness and access to cryospheric information and related data
- To facilitate the exchange of information between researchers, northern communities, decision makers, and the public.
What are the 3 spatial scales of snow cover distribution?
- Macroscale: 10-1000 km, influenced by larger scale meteorological effects
- Mesoscale: 100m-10km, distribution related to wind, terrain variables, and veg cover
- Microscale: 10-100m, distribution related to variations in air flow patterns and transport
Name a tool for measuring snow accumulation.
A snow pillow
What three factors affect water flow through snow?
- internal snowpack structure
- condition of the snowpack prior to introduction of water
- amount of water available at the snow surface.
What are the 4 liquid water regimes?
- Capillary: less than 1% free water. Capillary tension holds water
- Unsaturated: 1-14% free water. Gravity drains water, but air spaces continuous. Pendular Regime
- Saturated: > 14% free water. Gravity drains water, but air spaces discontinuous. Funicular Regime
- Melt/freeze: Water melts and refreezes, before draining from snowpack
describe basal ice development
On shallow slopes, ponded meltwater may refreeze at the base of the pack, forming ice layers that impede further meltwater infiltration
describe subnivean flow
Lateral flow of basal ponded water depending on slope. If snow still present, lateral flow is still through a porous medium. Presence of liquid water in base of snowpack causes rapid destruction of small snow grains, leaving larger grains, and allowing more rapid flow.
What are two mechanisms of snow accumulation on glaciers?
- snow fall
- low temperature
What are three mechanisms of snow ablation on glaciers?
- sublimation
- rain
- calving
What is the difference between primary and secondary permeability
Primary permeability occurs in intact ice and snow, particularly snow and firn with linked pore spaces.
Secondary permeability is tunnels and pathways, the primary meltwater routes in glaciers
What constitutes supraglacial flow?
streams, lakes, the snow aquifer
What constitutes Englacial flow?
crevasses, moulins, fractures
What constitutes subglacial flow?
channels, cavities, sheets, canals, groundwater
what is the difference between glacial flow on the surface versus at the base?
Surface flow is dependent on elevation, while base flow is dependent on elevation and pressure