GL 2 Flashcards

1
Q

What is the cryosphere?

A

Parts of the crust and atmosphere that are below zero degrees for a part of the year

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2
Q

How are icebergs formed

A

Broken of of glaciers into water via calving

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3
Q

What is permafrost

A

permanently frozen ground

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4
Q

What is the morphology of glaciers?

A

Form, shape and structure of ice

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5
Q

What two factors impact the morphology of a glacier?

A

Climate and topography of land

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6
Q

What is climate? And how does it impact a glacier’s morphology

A

Climate is contorlled by annual temperature cycle. Warmer climate causes negative mass balance vice versa.

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7
Q

What is topography? And how does it impact glaciers morphology?

A

Topography is the natural shape of the land. Land surface, e.g. altitude. Controls physical dimensions of the glaciers and how they can flow.

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8
Q

What is an unconstrained land mass?

A

morphology and flow pattern that is not fully dependent of the topography of land

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9
Q

What is a constrained ice mass?

A

Morphology and flow pattern that is strongly based on topography

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10
Q

Ice sheet:
Description, size, constrained or unconstrained?
Example

A

Topography is submerged in ice, forms gently sloping domes of ice several km thick. +50,000km2. Unconstrained. Antarctic ice sheet

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11
Q

Ice cap:
Description, size, constrained or unconstrained?
Example

A

Smaller version of an ice sheet. >50,000km2. Unconstrained. Vatnajökull ice sheet

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12
Q

Ice field:
Description, size, constrained or unconstrained?
Example

A

Ice covering upland area, does not bury topography. 10-10,000km2. Constrained. Patagonian ice fields

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13
Q

Valley glacier:
Description, size, constrained or unconstrained?
Example

A

Confined between valley walls, finishing in a narrow tongue, made from ice caps, sheets or cirques. 3-1500km2. Constrained, Aletsch glacier, Swiss Alps

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14
Q

Piedmont glacier:
Description, size, constrained or unconstrained?
Example

A

Valley Glacier that extends beyond end of a mountain into flat area, spreading out. 3-1000km2. Constrained. Malaspina, Alaska

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15
Q

Cirque glacier:
Description, size, constrained or unconstrained?
Example

A

Occupies a hollow on a mountain side, calves out a corrie. 0.5-0.8 km2. Constrained. Styggebrean Norway

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16
Q

Ice shelf/sea ice:
Description, size, constrained or unconstrained?
Example

A

Large area of floating glacier ice, many glaciers coalesce (fuse). 10-10,000km2. unconstrained. Larsen Ice shelf

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17
Q

What is thermal regime?

A

the temperature of the ice

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18
Q

What are the two types of thermal regimes, and what is the difference?

A

Cold based (polar glaciers) - Glacier is permanently frozen to ground. Average temperature is well bellow 0, surface temperature is -20 to -30. High latitudes.
Warm based (temperate glaciers) - Glacier is not frozen to bedrock. Temperature fluctuates to above melting point, causing meltwater, this is due to the pressure melting point (water melts due to high pressure, even while temperature is below 0 degrees celcius). High altitudes.

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19
Q

Why are glaciers able to move?

A

Glacial ice can deform

20
Q

What is pressure melting?

A

Ice melts at temperature below 0 degrees, due to pressure of overlying ice.

21
Q

What is the equation for pressure melting?

A

melting point falls at a rate of 1 degree Celsius for every 100kg/cm3 of pressure

22
Q

In what thermal regime do glaciers melt. Why?

A

Warm based glaciers reach pressure melting point at depth. Causing meltwater.
Cold based glaciers do not melt as temperature is far from pressure melting point all thought the glacier.

23
Q

What is Regelation

A

Ice melts under pressure, when pressure is relieved water refreezes

24
Q

Is Basal sliding warm based or cold based?

25
Q

What is Basal sliding? This is not a specific type of movement, all warm based glaciers do this.

A

Only occurs when there is meltwater, acting as a lubricant reducing friction, enabling movement.

26
Q

What is enhanced Basal creep? Cold or warm?

A

Glacier comes into contact with an obstacle. Ice deforms around obstacle, but does NOT reach pressure melting point. Warm based only.

27
Q

What is the Stoss and Lee side?

A

Stoss - up side
Lee - down side

28
Q

What is Regelation slip. Cold or warm?

A

f temperature of ice is close to pressure melting point, increased pressure from the stoss side (up movement) of glacier will induce melting. Glacier is able to slip and meltwater flows around obstacle to the Lee side, pressure is reduced and meltwater refreezes - linking to regulation. Warm only.

29
Q

What is internal deformation. This is not a specific type of movement, all warm and cold based glaciers do this.

A

individual grains of ice withing glacier responding to pressure, this is NOT melting. This is effected with ice thickness and slope angle.

30
Q

What is intergranular flow? Warm or cold based?

A

Displacement of ice grains relative to one another. Bottom grains are stationary while top rotate clockwise, this is due to slope angle as it is reliant on gravity. A steeper slope angle causes more movement. Warm and cold based.

31
Q

What is Laminar flow? Warm or cold based?

A

Layers of ice slipping over one another. Ice at the bottom has slower relative velocity then ice at top. This is due to slope angle as it is reliant of gravity. A steeper slope angle causes more movement. Warm and cold based.

32
Q

What is the deformation of ice called? What is it caused by? Warm or cold?

A

Ice creep. Caused by increased ice thick and/or slope angle. Warm and cold

33
Q

How does ice deformation cause ice faults, fractures and crevasses.

A

Ice is not able to deform quick enough

34
Q

Explain extensional and compressing flow.

A

When slope gradient is increased, ice accelerated, causing crevasses. This is extensional flow.
When slope gradient is decreased, ice slows down, causing ice behind to catch up, leading to ice thickening, and crevasses to close. This is compressing flow.

35
Q

What is subglacial bed deformation? Warm or cold based? What does this cause?

A

Glacier moves over weak, loose rock, causing sediment to deform under weight of glacier. Warm based glacier only.
In Icelandic glaciers this causes 90% of glacial movement

36
Q

What thermal regime glaciers move faster?

37
Q

What is the range of movement in a glacier per year?

A

3-300m per year

38
Q

How does slope angle impact velocity?

A

Higher slope angle = more velocity
vice versa

39
Q

How does thermal regime impact velocity?

A

Warm based glaciers have more velocity due to
- Water acting as lubricant
- More movement options
- Basal sliding

40
Q

What are glacial surges?

A

Periods of rapid movements

41
Q

How much faster can a glacier move in surge conditions?

A

Up to 1000 times faster

42
Q

What are glacial surges caused by?

A

change of flow pattern of subglacial meltwater

43
Q

Describe surge conditions

A

Water builds underneath glaciers. Increase of ice in accumulation zone. During winter subglacial meltwater channels are closed, increasing accumulation of ice. During summer ice accumulation is so great that subglacial meltwater channels do not open. Pressure melting point and subglacial meltwater separates basal ice from it’s bed, lubricating it and causing faster velocity. Abundant water increased pore water pressure, adding to movement, Surge occurs and glacier returns to normal flow.

44
Q

What case study is used for glacial surges

A

Muldrow Glacier, 2021

45
Q

When did Muldrow Glacier last surge? How far did it move?

A

1956, moving 4 miles

46
Q

How far did Muldrow Glacier move? How much more is this then normal? What did this cause?

A

200ft in 4 days, 10-20m in one day, 100x faster then normal, caused massive crevasses

47
Q

Where does Muldrow lie that impacts surge conditions

A

Lies on a fault line, which causes earthquakes