The Arctic Tundra Flashcards

1
Q

what are the climatic conditions?

A

for 8 or 9 months it has a negative heat balance with avg monthly temp below freezing, as a result the ground is permanently frozen with only the top metre thawing in summer
in winter temp can go below -40C
mean annual precipitation is low

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2
Q

what is the biodiversity like?

A

low - few plants + animals have adapted to this environment
treeless
in low arctic conditions are less severe + vegetation provides continuous ground cover

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3
Q

what are the main features of the water cycle?

A
  • low precipitation (50-350mm) most = snow
  • small stores of moisture due to low temp which reduce absolute humidity
  • limited transpiration due to sparseness of the vegetation cover + short growing season
  • low rates of evaporation ->. much of suns energy is melting snow so ground temp remains low
  • limited groundwater + soil moisture stores, permafrost is a barrier to infiltration, percolation, recharge + groundwater flow
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4
Q

what results in sharp increase in river flow?

A

melting of snow, river + lake ice + uppermost layer of the permafrost in spring + early summer

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5
Q

what are the main features of the carbon cycle?

A
  • permafrost is a vast carbon sink (global 1600 GT)
  • accumulation of carbon is bc low temp + slow decomposition of dead plant materials
  • flux of carbon concentrated in the summer when active layer thaws -> plants grow rapidly, long hours of daylight (but NPP is less than 200 grams/m2/yr)
  • growing season; tundra plants carbon rich litter to the soil, activity of microorganisms increases, releasing Co2 to the atmosphere through respiration
  • even in the winter pockets of unfrozen soil + water in permafrost act as sources of Co2
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6
Q

permafrost used to function as a carbon sink what do people think it is now?

A

carbon source

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7
Q

what evidence suggests that the arctic remans balanced in the carbon budget?

A

increase in outputs of carbon from permafrost but higher temp so growth of plants + greater uptake of Co2

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8
Q

how does temperature affect flows + stores of water?

A

avg temp are well below freezing so water is stored as ground ice in the permafrost layer
during summer the shallow active layer thaws + liquid water flows on the surface -> meltwater forms million of pools + lakes.
draining = poor, water cannot infiltrate the soil bc of the permafrost.
in winter sub zero temp prevents evapotranspiration
humidity is low all year round + precipitation is sparse

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9
Q

how does permeability affect flows + stores?

A

low owing to permafrost + the crystallin rocks which dominate the geology of the tundra in arctic

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10
Q

how does relief affect flows + stores?

A

gentle undulating plain due to 100 mill yrs of erosion + weathering
minimal relief + chaotic glacial deposits impede drainage + contribute to water logging during summer months

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11
Q

how long has the carbon been locked away for in the permafrost?

A

500,000 years

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12
Q

why is total carbon store of the biomass relatively small?

A

low temp, unavailability of liquid water + parent rocks contains few nutrients = limits growth

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13
Q

what slows decomposition + respiration?

A

low temp + water logging = limit flow of Co2 to atmosphere

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14
Q

what has little influence on the water + carbon cycle?

A

impermeability of the permafrost, rock permability, porosity + mineral composition of rocks

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15
Q

when were oil and gas discovered?

A

1968, prudhoe bay

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16
Q

what challenges did the development of oil + gas experience?

A
  • harsh climate -> extreme cold
  • permafrost
  • the melting of the active layer in summer
  • poor accessibility
17
Q

by 1990s what % of USAs oil production was from north slope?

A

25%

18
Q

what is the % of usa’s production today from north slope?

A

6%

19
Q

why did the production decline?

A

high production costs

massive growth of the oil shale industry in usa

20
Q

how has oil + gas production affected carbon + water?

A

permafrost is highly sensitive to changes in thermal balance -> balance has been disrupted which have caused localised melting of the permafrost
melting is associated w:
- construction + operation of oil + gas installations
- dust deposition along roadsides creating darkened snow surfaces this increasing absorption of sunlight
- removal of vegetation cover which insulates permafrost

21
Q

what does melting of the permafrost do? CC

A

releases Co2 + methane, on north slope estimated co2 losses from permafrost very from 7 mill to 40 mill tonnes per yr
gas flaring + oil spillages also input co2 into atmosphere

22
Q

what does the destruction or grading of tundra vegetation do?

A

reduces photosynthesis + uptake of co2 from the atmosphere + the thawing of soil increases microbial activity, decomposition + emissions of co2

23
Q

how does the slow growing nature of tundra vegetation affect recovery?

A

regeneration from damage could take decades

24
Q

how does the melting of permafrost affect WC?

A

increases run off, river discharge making flooding more likely
in summer wetlands, pools etc have become more extensive, increasing evaporation

25
Q

how has drainage been disrupted?

A

strip mining of sand + gravel -> also exposes permafrost to further melting
also disrupted by road construction + seismic explosions u

26
Q

strategies to reduce the impact of development on the water + carbon cycle

A

insulated ice + gravel pads -> protecting permafrost from melting
buildings + pipelines elevated on piles -> allows cold air to circulate structures
drilling laterally beyond drilling platforms -> allows oil + gas to be accessed several km from drilling sit -> fewer sites needed -> impact on vegetation + permafrost is reduced
refrigerated supports -> used on trans-alaska pipeline to stabilise temp