Thermokarst Processes Flashcards

1
Q

What happens when permafrost thaws on slopes?

A

Thermokarst slumps- river or sea cliffs, unconsolidated, naturally exposed to sun/air/water and thus potential to thaw.

Back-wearing: slumps occur as ground ice thaws and sediment flows- occurs along riverbanks and sea cliffs: open faces exposed to sun, air, rain. c

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2
Q

What is “liquid limit”?

A

Amount of water needed to liquefy the surface sediment.

If excess ice > liquid limit, thermokarst will generate sediment flow- sediment lost alone.

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3
Q

What do thermokarst lakes require?

A

Unconsolidated sediments to have accumulated. Rare in glaciated landscapes.

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4
Q

How does thermokarst occur?

A

Excess ice = water locked in large ice bodies

Thawing leads to overall loss of volume (ice to water)

Super saturated (more water than available pore space) leads to collapse and/ or flow-age

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5
Q

What are syngenetic ice wedges?

A

Grow as substrate accumulates over time (e.g loess).

Wind blown sediment.

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6
Q

What is an ice complex?

A

With holey cheese, imagine the holes are filled with silt and the cheese is ice and the ice gets eroded away.

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7
Q

Climate and disturbance-generated thermokarst

What does a mean warming of the environment change?

A

Everything under the ground changes its temperature regime if above the grounds temperature changes.

Cold -> hot = get an increase in depth of thaw (active layer thaws deeper).

Generate melting of ice.

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8
Q

What are some effects of disturbance on thermokarst?

A

Removal of insulating vegetation (including forest moss layer) or thinning/ loss of peaty soil can lead to more surface heating and enhance thermokarst.

Fire severely affects resilience of landscape to thermokarst.

Warming plus more/ severe fire may lead to a tipping point, where permafrost is permanently degraded.

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9
Q

What are some human induced thermokarst disturbances?

A

Emplacement of infrastructure, forest clearance, roads and tracks can all disturb the surface heat budget and affect the active layer.

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10
Q

How is methane generated in thermokarst lakes?

A

Deep aeolian sediments containing carbon.

Inside thaw bulb is >0oC and anaerobic decomposition f carbon leads to methane production.

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11
Q

Summary: when does thermokarst occur?

A

When ice rich ground is subject to a change in conditions that encourage thaw (disturbance, climate change).

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12
Q

Summary: what does excess ice lead to?

A

Thaws and leads to loss of mass, karsting and slumping.

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13
Q

Summary: what happens if liquid limit exceeds sediment flows?

A

Rapid erosion (sea, cliffs, river banks)

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14
Q

Summary: what is it that gives rise to lakes of different depths?

A

Shallow epigenetic wedges and deep syngenetic wedges may thaw in level ground.

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15
Q

Thermokarst: sequences of landscape transformation

A
Disruption of land surface
Usually increase in wetness
May form ponds -> lakes
Changes in shape and depth can be rapid
Enhanced emission of methane to atmosphere
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16
Q

Draining can lead to

A

Terrestrialisation (some drawdown of carbon by vegetation and peat growth).

Pingo growth (sometimes)

New ice wedges

New pond formation