G&H3: Hydrology Flashcards

1
Q

3 reasons why glacier hydrology is important?

A
  1. glacier fed rivers provide large % of agriculture water supply
  2. hydropower
  3. potential hazard
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2
Q

What are the inputs to the glacial hydrological system?

A

Snow, rain, valley-side runoff, surface melt, basal melt

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3
Q

What are the two storage types of the glacial hydrological system?

A
  1. snow and ice

2. lakes

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4
Q

What are the 3 transport types of the glacial hydrological system?

A

supraglacial channels
englacial conduits
subglacial drainage

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5
Q

What is the relative permeability of snow, firn and ice?

A
snow = highly permeable
firn = permeable
ice = inpermeable
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6
Q

What is a way to think of how permeable firn is and how this affects its storage/

A

It is like a slush puppy

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7
Q

Because ice is impermeable, what does this cause overlying water to do

A

it becomes runoff that will incise supraglacial channels and consequently infill supraglacial lakes

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8
Q

What is hydraulic potential?

A

The pressure/power of the hydrology like how powerful the water body is

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9
Q

How does water flow with hydraulic potential?

A

Water flows down lateral gradients of hydraulic potential. It will flow down the steepest slopes of hydraulic potential and will also flow fastest down these areas

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10
Q

How are supraglacial lakes formed?

A

the surface runoff will collate in an ice surface minima where the inflow>outflow. As the inflow is greater the lake will consequently keep growing in area

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11
Q

What can happen once a supraglacial lake grows big enough that it encounters a crevasse in the surface?

A

the lakes can drain very quickly if they encounter a crevasse because it is essentially a weak point in the ice and so if the pressure from the ever-increasing water body grows then this crevasse will collapse forming a vertical drain from the surface down below.

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12
Q

What is the name given to a vertical drain from the surface down to a crevasse?

A

Moulin

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13
Q

What is the name given to the process of vertical draining through a moulin and what does it involve?

A

hydrofracturing - as the water drains quickly through the moulin the ice the friction against the ice will cause greater melting and stretching of the drainage hole

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14
Q

What are some possible drainage destinations from a moulin?

A

glacier base, englacial channels, conduits

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15
Q

Why is there uncertainty regarding the routing of drained supraglacial water?

A

Because we are unable to access the base of the glacier safely and so conducting investigations is less easy

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16
Q

What study is much of the minimal knowledge regarding englacial/subglacial processes inferred from?

A

Shreve (1972)

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17
Q

What did Shreve (1972) state?

A
  1. englacial drainage systems are in a steady state where by glaciers are constantly trying to close up on themselves but the glacier hydrological flow is resistant against
  2. englacial water flows along the steepest hydraulic gradient
  3. pressure head (the pressure on the walls flowing through the channels) is the pressure of surrounding ice of channels minus melting of walls
18
Q

Where have most investigations in to englacial/subglacial processes been focused?

A

Svalbard

19
Q

What key component changes between supraglacial and supraglacial environments?

A

Presence of ice overburden pressure

20
Q

What is the ice more likely to reach as a result of the greater pressure exerted upon it?

A

Pressure melting point

21
Q

What do we assume the pressure of the water at the base of the ice to be?

A

The ice overburden pressure

22
Q

What can sometimes happen to water as a result of the overburden pressure which would usually be regarded as unusual?

A

The water can flow uphill

23
Q

Where would upward flowing water at the base of the glacier most commonly be found and why?

A

further away from the glacier outlet because closer to the glacier outlet means that the ice thickness decreases and so the overburden pressure also does

24
Q

What can a relic upward flowing channel tell us about past glacial landscapes?

A

that the ice was of a great enough thickness to cause water to flow upwards

25
Q

What are the two types of subglacial drainage?

A

Channelised and distributed

26
Q

What are the two types of channelised subglacial drainage?

A

Rothlisberger channel and nye channel

27
Q

What are rothlisberger channels and how are they formed?

A

They are channels that have been created by erosion in to the base of the ice as a result of the ice overburden pressure subsiding enough to allow the channel to erode upwards. Because of this the channels are most commonly found near the glacier outlet where the pressure is less

28
Q

What is the balance between ice overburden pressure and hydraulic potential at rothlisberger channels?

A

ice overburden < hydraulic potential

29
Q

What will happen to rothlisberger channels usually at the end of summer and why?

A

They will be forced to close up because of the diminishing supply of water to the base of the glacier that will reduce the hydraulic potential of the water and so the overburden pressure will exceed it. This happens at the end of summer because ablation starts to tail off at the end of this season

30
Q

What happens at the tunnel boundary of the rothlisberger channels?

A

Overburden pressure = hydraulic potential and so any changes to either will affect the shape of the tunnel

31
Q

What are nye channels and how are they formed?

A

These are channels created in the sediment/bedrock below the ice because the ice overburden pressure buries the channel to force erosion happening downwards

32
Q

When is a nye channel more likely to be preserved?

A

if the channel is eroded in to underlying bedrock as opposed to sediments because the latter are more easily reworked over time

33
Q

What are water films and when are they caused?

A

Thin layers of water at the base of usually a temperature ice body which is prone to basal melting which provided a supply of water to the base of the glacier

34
Q

Why is it hard to observe water films?

A

because they exist at the base of a glacier which is hard to access

35
Q

What is a water film limited in its ability to do?

A

transport material because it is such a small amount of water

36
Q

What is a water film fundamental for?

A

Regelation which is effectively what permits glacier basal sliding

37
Q

What is a linked cavity system and how do they occur?

A

water-filled cavities at the bed of a glacier where basal pressure exceeds the local ice pressure. The cavities allow for greater basal motion which creates more cavities thereby forming a positive feedback

38
Q

What is groundwater flow?

A

water flowing through sediments below the glacier, only sediments.

39
Q

What determines the amount of water flow through these sediments and how?

A

Darcy’s Law - this calculates the likely discharge of water through a material

40
Q

What is likely to be the groundwater flow through poorly sorted sediments and well sorted?

A

Poorly sorted sediments are impermeable so groundwater flow will be minimal but for well sorted sediments this is reversed.