L20 Flashcards

1
Q

What is permafrost?

A
  • Ground frozen for at least two consecutive years
    • 24% of land in northern hemisphere
    • Mostly high latitudes but some alpine areas too
    • Permafrost stores carbon as peat and soil organic matter & methane
    • 1300 Gt of carbon stored in permafrost, more than twice as much C than the atmosphere
    • Permafrost is thawing - there are carbon release issues with this
    • Permafrost zones (continuous, discontinuous and sporadic)
    • Permafrost thaws but never melts - eg includes rocks
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2
Q

How much of land in the Northern hemisphere is permafrost?

A

24%

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3
Q

How much carbon is stored in permafrost?

A

1300 Gt - more than twice as much C than the atmosphere

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4
Q

The active layer

A
  • Surface that thaws each summer (re-freezes in winter)
    -Permafrost thaw from climate warming
    -Active layer gets progressively deeper
    = active layer thickening/ deepening
    • Permafrost is below the active layer
    • Permafrost is thawing due to warmer temperatures, more permafrost is becoming part of the active layer
    • Exposes more carbon to decay previously preserved in the permafrost
  • Positive feedback to climate (not good)
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5
Q

5 Ecosystem controls of active layer thickness

A
  1. Evergreen trees (vs deciduous)
  2. Moss cover (winter vs summer heat transfer)
  3. Shrub/ understorey cover (shields irradiance)
  4. Organic (peaty) soils
  5. Dry soil
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6
Q

Evergreen trees (vs deciduous)

A
  • Winter canopy snow trapping
  • Stopping snow insulation and help to keep the ground cool
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7
Q

Moss promotion

A
  • Protects permafrost
    • Moss is dry in summer so insulates and keeps summer heat away
    • It is wet in winter so conducts heat and transfers heat out of the ground to the atmosphere
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8
Q

Dry soil

A
  • Drainage
  • Precipitation vs transpiration
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9
Q

Large scale ecological relationships

A
  • Walker et al 2003

-Transect through northern alaska

-Thaw depth does not get deeper
-North- south changes ecosystem characteristics that affects permafrost
-Larger and leafier southern plants shades and keeps ground dry, so protects permafrost and counters the warmer temperature

-No relationship between active layer depth and temperature

-Demonstrates ecosystem characteristics importance as they counter the warmer climate to protect the permafrost

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10
Q

Ecosystem controls on ALT

A

-Tree canopy leaf area
-Understorey leaf area
-Understorey height
-Moss depth
-Soil organic layer depth
-Soil moisture at surface
-Soil moisture at depth
-% cover of plant species

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11
Q

Birch ALT

A
  • Large
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12
Q

Large spruce ALT

A
  • Small
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13
Q

What increases ALT?

A

Burning - this is bad for permafrost

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14
Q

Why is burning bad for permafrost?

A

-Heat of fire is little effect, main effect is canopy and moss loss so no protection

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15
Q

A thicker moss layer result in…?

A

A shallower ALT

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16
Q

A thicker organic layer results in…?

A

A shallower ALT

17
Q

Which is more important for ALT, moss thickness or organic matter thickness?

A

Moss

18
Q

Tree canopy LAI

A
  • Of some importance
  • Only surface moisture increases with fire
19
Q

Interaction of ecosystem characteristics

A

-Steep sites have least influence of organic thickness
- shallower sites organic thickness is more important
- Good drainage on steeper slopes probably lessens importance of insulating organic layer
- Tree canopy leaf area has a much lesser influence in drier soils
-Shading of irradiance less important when you have dry soils that insulate well

20
Q

Methane flux and permafrost thaw

A
  • Subsidence of the ground when ice thaws
    • This can then be filled with water and create a wetland

Thermokarst Wetlands produce high methane, little of this comes from old C formerly locked in permafrost

Methane emissions is thought to be ¼ of permafrost associated global warming

Methane emissions increase with biological activity
-Similar amounts of methane emitted from centre of wetland vs outer of wetland (new)
- Long term capacity to keep emitting methane
- Consistent emissions

21
Q

Methane emissions account for what % of permafrost global warming?

A

1/4

22
Q

Methane dating experiment

A

-Deepest methane is thousands of years old
- Methane has been made from permafrost carbon
- Permafrost melting must supply carbon

23
Q

Surface methane

A
  • Isn’t dominated by old carbon
    • Only 8% of carbon in surface methane is from old deep stores in permafrost
    • Wetlands do not release large amounts of carbon than then contribute to methane emissions
  • Methane arises from recent carbon not long term carbon stores