CASE STUDY: The Arctic Tundra Flashcards

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1
Q

background facts on AT

A
  • AT occupies some 8,000,000km2 in northern Canada, Alaska + Siberia
  • av. monthly temps =regularly below freezing
  • few flora + fauna have adapted to these conditions so biodiversity is low
  • permafrost underlies much of the tundra
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2
Q

main features of the AT water cycle

A
  • low annual precipitation: 50-350mm/year
  • low rates of evaporation as Sun’s energy used for melting snow + surface/soil waters are mostly frozen
  • limited groundwater + soil moisture as permafrost blocks infiltration, percolation + groundwater flow, so extensive wetland, ponds + lakes during summer due to permafrost preventing drainage
  • limited transpiration due to sparseness of vegetation + short growing season
  • accumulation of snow + river/lake ice during winter - melts in spring + summer = rapid increase in river flow
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3
Q

the permafrost in the AT is a vast…

A

carbon sink

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4
Q

how much greater is the amount of carbon in tundra soils than in above-ground biomass

A

the amount of carbon in tundra soils is 5x greater than in above-ground biomass

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5
Q

why is the flux of carbon concentrated in the summer months in the AT

A
  • flux of carbon is concentrated in summer months, when active layer of permafrost thaws
  • during summer growing seasons, tundra plants input carbon-rich litter to soil. activity of micro-organisms increases, releasing CO2 to the atmos. through respiration
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6
Q

how are CO2 and CH4 emissions not limited to summer months alone

A
  • even in winter, small pockets of unfrozen soil + water in permafrost act as a source of CO2 + CH4
  • meanwhile, snow cover insulates some microbes, allowing decomposition to continue even at very low winter temperatures
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7
Q

what concerns surrounding global warming and permafrost exist?

A

in the past, permafrost functioned as a carbon sink; but today, global warming has raised concerns that permafrost is becoming a carbon source

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8
Q

why is the release of methane particularly worrying, but how can this be countered and how can it be possible that the AT’s carbon budget is balanced

A
  • the release of methane is particularly worrying as it can trap 30x as much heat as CO2
  • however, higher temperatures have also stimulated plant growth = increased uptake of CO2 for photosynthesis as well as increasing the carbon store of plant litter
  • It is thus possible that AT’s carbon budget remains balanced
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9
Q

what is carbon mainly stored as, where and for how long (in AT)

A
  • carbon is mainly stored as partly decomposed plant matter frozen in the permafrost
  • most of this carbon has been locked away for the past 500,000 years
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10
Q

what is carbon flux

A

the amount of carbon exchanged between Earth’s carbon sinks (eg. atmosphere, oceans)

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11
Q

what is biomass

A

the total quantity or weight of organisms in a given area or volume

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12
Q

when were oil + gas discovered in the North Slope of Alaska

A

oil + gas were discovered in the North Slope of Alaska in 1968

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13
Q

What did the USA do in the 1970s + 80s with ref. to the North Slope and why

A
  • in the 1970s + 80s, massive investments went ahead (into oil pipelines, production plants, gas processing facilities, etc.)
  • this was driven by high global energy prices + the USA’s attempt to become more oil independent
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14
Q

How much of the USA’s domestic oil production did the North Slope account for by the early 1990s (+ today?)

A

By the early 1990s, the North Slope accounted for nearly 1/4 of the USA’s domestic oil production (today still around 6%)

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15
Q

what significant impact on permafrost has the oil + gas exploitation of Alaska’s North Slope had and what has caused this impact specifically

A
  • oil + gas exploitation on Alaska’s North Slope has had a significant impact on permafrost
  • localised melting of permafrost has been caused due to:
  • construction of oil + gas installations diffusing heat directly to environment
  • dust deposition on roadsides creating darkened snow surfaces, thus low albedo (poor ability to reflect sunlight) increasing sunlight absorption
  • removal of vegetation cover which insulates permafrost
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16
Q

impacts on carbon cycle (STATS)

A
  • permafrost melting releases CO2 + CH4
  • on the North Slope, CO2 losses from permafrost = 7-40million tonnes/year + CH4 losses from permafrost = 24-114 thousand tonnes/year
  • gas + oil spillages release CO2 into atmos.
  • industrial development - destruction of vegetation = decrease in photosynthesis + NPP
  • thawing of soil decreases microbial activity therefore increasing CO2 emissions from decomposition
17
Q

impacts on water cycle

A
  • melting of permafrost + snow cover increases runoff + river discharge = high flood risk
  • in summer, due to melting of permafrost + global warming, wetlands, ponds + lakes become more extensive, increasing evaporation, increasing moisture in atmos., increasing precipitation, increasing vegetation, increasing evapotranspiration
  • mining of sand/gravel creates artificial lakes, disrupting drainage + exposing permafrost to further melting
  • water abstracted from creeks + rivers for industrial + building of ice roads reduce localised runoff
18
Q

what is the NPP in AT and why is it low?

A

NPP is low (200g/m2/year) due to little vegetation + short summer so limited photosynthesis

19
Q

what is the ‘active layer’ of permafrost

A

the top metre of the permafrost which thaws during the summer months

20
Q

how many GT of carbon does the permafrost contain globally

A

globally permafrost contains 1600GT of carbon