Glacial Processes and Landforms Flashcards

1
Q

How much of the world’s freshwater is stored in the global cryosphere?

A
  • 75 percent
  • Short time scales in snow, rivers and lake ice, sea ice
  • Short and long time scales in glaciers and ice caps, frozen ground
  • Short to long timescales in ice sheet margins to ice shelves to ice sheets
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2
Q

How much would global sea level rise if all of the ice in Antarctica melted? Greenland?

A
  • Antarctica: 58m

- Greenland: 7m

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3
Q

Thermal expansion and mountain glacier melt (not greenland/antarctica) explain how much of the observed sea level rise since 1971?

A
  • 75 percent

- Thermal expansion will be the biggest contributor to SLR, followed by mountain glacier melt

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4
Q

Percent of global land surface from most to least for ice on land

A
  • Seasonally frozen ground 33
  • Terrestrial permafrost 9-12
  • Antarctica 8.3
  • Greenland 1.2
  • Northern hemisphere freshwater (lake/river) ice 1.1
  • Glaciers 0.5
  • Snow cover 1.3-30.6 (highly variable
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5
Q

In all climate change scenarios, what is the largest contributor to SLR projections? Which one gets the press?

A
  • Thermal expansion is largest contributor

- But melting glaciers gets all the press b/c is more visually spectacular even though it only comes in second

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6
Q

Glacier size and reaction times

A
  • Ice sheets, 1000m thick, 100km long, reaction time 1000yrs
  • Valley glaciers, 100m thick, 10km long, 100yr reaction time
  • Cirque glaciers, 10m thick, 0.1km long, 10yr reaction time
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7
Q

What are the 2 criteria for a glacier?

A
  • Perennial accumulation of snow and ice

- Flows under it’s own weight

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8
Q

How are glaciers classified by?

A
  • Morphology (size)
  • Flow dynamics
  • Thermal properties
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9
Q

Snow to ice density

A
  • Increases in density w/ depth in glacier
  • Fluffy snow 0.05-0.2 g/cm3
  • Firn 0.4-0.8 g/cm3
  • Glacial ice 0.8-0.9 g/cm3
  • Pure ice 0.917 g/cm3
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10
Q

Mass Balance, Bm

A
  • Glacier’s chequebook
  • Balance btwn inputs/accumulation and outputs/ablation of snow, ice, water and vapour
  • Most of world’s glaciers are negative, but only few are monitored
  • If Bm > 0, glacier grows, advances terminus
  • If Bm <0, glacier shrinks, terminus retreats
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11
Q

How many glaciers are there worldwide?

A
  • 170,000

- Even in Africa on Mt Kiliminjaro (16 ice fields) and 2 other Mnts

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12
Q

How is the Mass Balance accounted for?

A
  • Whole year gives balance, mean water equivalent

- Can’t look at just summer b/c negative or winter b/c positive

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13
Q

Equilibrium line altitude (ELA)

A
  • Elevation where no net gains or losses of water occurs
  • Connected to local climate (change)
  • Same as firn line in late summer/early fall
  • Controlled by temp and precip
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14
Q

Thermal classification of glaciers

A
  • Ice temp important to control flow
  • Polar/cold glaciers
  • Temperate/warm glaciers
  • Subpolar/polythermal glaciers
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15
Q

Pressure melting point, PMP

A
  • Water melts/freezes at 0C at 1 atm pressure
  • But PMP decreases w/ increasing pressure
  • i.e. Melts at a lower temperature than 0C at higher pressure
  • Declines by 1C for every 14MPa
  • ex. 20MPa = PMP approx. -1.6C
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16
Q

Polar/cold glaciers

A
  • Temp &laquo_space;PMP

- Frozen to bed (at least at margins)

17
Q

Temperate/warm glaciers

A
  • Temp at approx. PMP throughout

- Water at bed

18
Q

Subpolar/polythermal glaciers

A
  • Parts of glacier at PMP temp and other parts not

- Most pleistocene ice sheets were polythermal

19
Q

Continental size/morphology classification

A
  • Ice sheet, > 50,000 km2 that buries landscape
  • Ice cap, < 50,000 km2 that buries landscape
  • Ice shelf, floating ice anchored to land mass
20
Q

Transitional size/morphology classification

A
  • Outlet glacier, bounded by ice-free ground at margins
  • Ice stream, bounded by ice at margins
  • Piedmont glacier, valley glacier that exits mountain onto flat ground
21
Q

Alpine size/morphology classification

A
  • Ice field, not domed like cap or shelf
  • Valley glacier, ice flowing down valley
  • Cirque glacier, ice occupying hollow in bedrock that it formed
  • Niche glacier, ice occupying hollow in bedrock that it didn’t form
  • Surge-type glacier, sub-category which move very rapidly for short periods of time
22
Q

Pemberton icefield

A

300km2

23
Q

Columbia icefield

A

325km2

24
Q

Jakobshavn Isbrae, Greenland

A
  • Outlet glacier fed by ice stream
  • Flowing up to 15km/yr, in rapid retreat
  • Fastest glacier in the world
  • Accounts for approx. 4 percent of avg. 20th century rate of SLR
  • Warmer conditions increase melt and lubrication at base, increase speed
  • Warmer winders allow iceberg calving and high flow rates to continue
25
Q

Glacier flow mechanisms

A
  • Internal deformation
  • Basal sliding, if warm based
  • Subglacial bed deformation
  • Top part of glacier is passive, not contributing to flow, goes along for the ride