Snow Hydrology Flashcards
(39 cards)
Stamp Sands
left-over copper mine, use it on roads on snow
Importance of Snow
what’s society used to, preparation, economics, recreation, transportation, property damage, replenish water storage
Snow Hydrology
understanding and predicting the physical process of snow accumulation (how much), ablation (reduction), and melt water runoff (where ends up)
Snow Hydrology Issues
quantity of water in snow packs, magnitude and rate of water lost by sublimation, timing rate & magnitude of snow melt, and rate of melt water
Snow Crystal Formation
different temps form different crystals
Why does snow look blue?
reflects off of sky (which is blue); shortwave radiation
Lake Effect
Causes bands of snow
Snow Cover Distribution Types
Macroscale, Mesoscale, Microscale
Macroscale
distances 10-1,000 km (here to Raystown)
Mesoscale
distances 100 m to 10 km (Huntingdon)
Microscale
distances 10-100 m (here to baseball field)
Effect of Topography on Snow Distribution
depth increases with elevation (more snowfall events and lower evaporation/melt), but not only elevation; must consider other factors (slope, aspect, temp, vegetation, etc.)
Aspect
direction you’re facing
Effect of Vegetation on Snow Distribution
turbulent air flow above and within canopy, direct interception of snow by canopy elements; related to type, density, and nearby areas
Effect of Forested Environments on Snow Distribution
conifers are efficient interceptors, and cohesion makes it last longer, more accumulation in clearings (difference occurs during storms & caused by sublimation and interception)
Effect of Open Environments on Snow Distribution
relative accumulation on different landscapes in open grassland
Open Environment
highly exposed terrain, differences in vegetation/terrain produce variation in accumulation
Hydrologic Influences of Blowing Snow
redistribution of snow water equivalent & loss of water by sublimation
Blowing Snow Transportation
creep (roll), saltation (bounce), turbulent diffusion (suspended)
Blowing Snow: Sublimation Losses
snow particles more exposed to atmosphere during wind transport; depends on transport rate and distance, temp, humidity, wind speed, solar radiation
Snow Pack
porous medium (ice + air + liquid water), layers of different types, ice in crystals/grains bonded together, gets stronger with more compaction
Snow Pack SWE
snow depth x (snow density/water density); height of water if snow cover melted
Snow Pack Grain Size
average size of characteristic grains within a mass of snow (mm)
Snow Pack Temperature
variation of temperature between top and bottom (temp gradient & largely determined by thickness and mean surface temp) OR no temp gradient (isothermal)