Meltwater Pathways Exam Flashcards

1
Q

What is always operating together in a glacier?

A

Water in it’s frozen and liquid state within a glacier is always operating together.

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2
Q

Where does melt come from?

A

Surface melt

As the glacier moves, it generates internal heat which causes internal deformation.

As the glacier moves over the bed basal friction occurs.

Geothermal heating

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3
Q

What are the pathways of water?

A

Surface- supra glacial
Inside- englacial
At the bed- subglacial

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4
Q

What are moulins?

A

Large pothole that goes straight down to the bed.

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5
Q

What are cut and closure channels?

A

Supraglacial streams cut downwards and creep closes the roof on them.

(Gulley et al, 2015)

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6
Q

What are the subglacial water pathways?

A
• Channels/Conduits
– R-channels (Rothlisberger, 1972)
– N–channels (Nye, 1953) (cut into bed rock)
– Canals (Clark and Walder, 1994)
– Braided system
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7
Q

What are linked cavities?

A

Glacier will move away from the bumps on the leeside and leave an air filled gap (cavities)

Eventually water will be able to flow through the wall (linked cavities).

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8
Q

What are canals?

A

Broad flat channels where you have a glacier resting on a deforming bed, instead of having dentritric R channels you get canals.

Braided drainage network.

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9
Q

What is the concept of water film in subglacial water pathways?

A

Weertman (1972) suggested that all warm-based glaciers floats on a 1mm thin water layer.

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10
Q

What is the concept of water sheet in subglacial water pathways?

A

Creyts and Schoof (2008) suggest you could have a thicker layer, where the glacier rests on class (macroporous).

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11
Q

What are the two types of flow systems?

A

Fast systems

Slow systems

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12
Q

What are fast systems?

A

Channelized dendritic system (mostly R)

Low water pressure- water is collecting in channels and flowing through

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13
Q

What are slow systems?

A

Distributed system

High water pressure

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14
Q

Seasonal evolution of the hydrological system

A

In Arolla, early in the season, flow is in linked cavities, but later in the season flows in conduits

In mid-may, sun starts to shine on glacier… linked cavities start filling up

As seasons go on, more ice is melted, goes into glacier, goes through system, at first fills up- linked, eventually they flow in conduits.
Nienow et al (1998)

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15
Q

Spring Event

A

Links winter and summer- glacier suddenly speeds and rise up on a day that marks the spring.

Typical of warm based alpine galciersl

During the spring, meltwater builds up in the cavities, then suddenly the water passes a threshold, and the cavities are linked

So much water the glacier will lift off the bed- bed separation occurs

Glacier is uplifted and velocity increases

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16
Q

Water stored in winter,early spring, released in summer (Stenborg, 1970; Willis et al, 1993)

In winter passages are constricted so any ablation goes into storage, which is later released
Where…?

A
  • Fountain et al(1998) suggest that cavities too small, so water must be stored englacially
  • Murray et al (2000) found from Falljökull, water was stored in veins and lenses smaller than 10cm
  • At Black Rapids and Fels glacier (Raymond et al., 1995). 80-90% of the water carried in ‘slow systems’ the rest in ‘fast’ systems.
17
Q

Storage and glacier motion

A

Different system at Skálafellsjökull
Spring and autumn – subglacial fast system
Summer – 50% water goes into storage
Winter–water comes out of storage to produce the largest annual discharges

18
Q

Eskers

A

Sedimentary effects of water in a glacier
Eskers form from conduit sedimentation
Long sinuous ridges composed of sand and gravel
1-20m wide, 1-30m high, >100 m length

19
Q

What are R channels?

A

These are semi-circular channels cut upward into the ice.

20
Q

What are N channels?

A

Those incised into bedrock, perhaps suggesting long-term channel stability under some glaciers.

21
Q

In a typical alpine day where does the majority of…
The supraglacial component come from?
The subglacial component come from?

A

Sun and rain

Basal friction

22
Q

Seasonal evolution of a hydrological system such as Arolla

A

In winter, early in the season, flow is in linked cavities- DISTRIBUTED SYSTEM.

Later in the season (mid may) sun starts to shine, snow melts off.

Starts to fill up linked cavities to then flow in conduits- CHANNELISED SYSTEM.

23
Q

Seasonal evolution simplified

A

Winter (distributed system) -> Spring event -> Summer (channelized system)