Glaciers (mostly) Flashcards
(37 cards)
average yearly slr
3.5 - 4 mm/ yr
how many glaciers on earth
over 270 000
geodetic method of measuring glacier mass change
looks at elevation change, and calculates mass change using density assigned to firn, ice and snow
gravimetric method
using GRACE sat, measures direct mass change
coarse resolution
difficult to seperate from different mass change signals such as hydrological storage and GIA
how much land surface do glaciers cover
700 000 square km (0.5%)
What is the sea level equivalent of total glacier ice
0.41 m (170 000 cubic km)
mass balance
difference between the amount of ice and snow gained and lost by a glacier over a period of time
gigatonne
1 x 10^12 (1 cubic km of water)
How much ice melt needed to raise sea level by 1mm
361.8 Gt
Specific mass balance
mass lost or gained per unit area often in kg/m^2 or m.w.e (Metre Water Equivalent)
Sublimation
When solids transition directly to gas - occurs in ablation zone
what are the 2 drivers of Antlantification of the arctic?
atmospheric forcing and ice ocean interaction
Dynamic process of mass loss
involves ice - ocean interaction as opposed to surface process of mass loss
What is the percentage contribution of surface processes to global glacier mass loss?
90%
The remaining 10% is attributed to dynamic processes
What region is the largest global contributor of glacier mass loss?
Alaska - mostly due to atmospheric forcing
What process contributes the most to mass loss in mass loss in Patagonia
Neither, It’s roughly a 50/50 split between dynamic and surface processes
- Dynamic is mostly due to the Patagonian ice field and proglacial lakes
What is the trend of hypsometric control on glacier mass change?
At higher elevations there is less change
What is the number one contributor to slr in the cryosphere
glaciers
what is ASTER remote sensing
stereo photogrammetry
What does cryosat use
radar altimetry
What does icesat use?
lazer altimetry
What are models useful for
determining which physical processes are the most responsible for observed behaviour
Inferring quantities that are not directly observable
Forms of accumulation on glaciers
snowfall,
deposition of hoar/ freezing rain,
gain of snow by wind,
avalanching,
basal freeze,
internal accumulation/ refreezing
Forms of ablation
Melting,
calving,
wind blowing snow off glacier
avalanching
sublimation