G&H1: Mechanics Flashcards

1
Q

5 accumulation inputs

A

Snowfall, wind-blown drift, avalanches, condensation, surface water freezing

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2
Q

What is rime?

A

condensed moisture that transforms from gas to solid and bypasses the liquid phase

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3
Q

accumulation requirements

A

Sub-zero temperatures
atmospheric moisture
mountains and mountainous regions (prefferably)
(local variations)

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4
Q

What is the actual process of accumulation known as?

A

Firn compaction.

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5
Q

What is firn?

A

any H20 substance between the snow and ice phase

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6
Q

What is the density of snow, firn and ice?

A
snow = 5-300kgm-3
firn = 400-830kgm-3
ice = 917kgm-3
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7
Q

What is the density of ice similar to?

A

water (997kgm-3)

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8
Q

ablation outputs

A

calving
melting
evaporation/sublimation

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9
Q

What is sublimation?

A

transition from solid ice to gas that again bypasses the liquid phase

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10
Q

Steady state concept

A

glaciers are in an equilibrium between seasonal variations fluctuations. If they are perturbed outside of this equilibrium then the equilibrium will adjust

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11
Q

What would happen to the steady state if temperatures suddenly rose?

A

The glacier would retreat over a long timer period with seasonal variations during this long term retreat. Eventually the glacier would stop retreating and this new position would mark the boundary of the new glacier at which the seasonal variation would then fluctuate around

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12
Q

What is the driving stress?

A

The total pressure or tension exerted upon a glacier.

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13
Q

What is the role of the driving stress?

A

The stress will force the glacier to move/ will drive it forward or backward

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14
Q

What is the calculation for driving stress?

A

= Pi (ice density CONSTANT) x g (Gravitational CONSTANT) X H (glacier height) x SinA (A is the slope of the glacier)

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15
Q

What happens to the driving stress if the glacier slope angle is 0?

A

There is no driving stress because the glacier is flat

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16
Q

What is the key control on the driving stress of the glacier?

A

slope

17
Q

What are the 3 glacier motion mechanisms?

A

1) internal ice deformation (Uf)
2) sliding at the bed (Us)
3) shear in underlying deformable sediments (Ud)

18
Q

What is the internal ice deformation?

A

the glacier body is forced to flow as a result of driving stress causing ice deformation. the rate of deformation is dependent upon the driving stress.

19
Q

what law governs the internal ice deformation and how?

A

Glen’s Flow Law. This law dictates the viscosity of the ice which therefore determines how much the ice deforms

20
Q

What is sliding at the bed?

A

The glacier is able to slide over the bed

21
Q

What determines the rate of basal sliding?

A

whether the glacier is frozen to the bed, the bed roughness (friction), amount of entrained debris (sandpaper effect), availability of water at the bed (lubrication)

22
Q

What is shear in underlying deformable sediments?

A

Think of the bed underneath the glacier as a series of logs that roll as the glacier moves thereby also facilitating that movement of the glacier

23
Q

What affects the amount of deformable sediments?

A

water content and pressure of sediments. High pressure means that the sediments are weak and therefore very deformable

24
Q

Why is deformable sediment movement not known much about and how do we know what we currently know?

A

Because the bed is hard to access and so we use models to simulate the bed to provide information