L18 Flashcards

1
Q

Boreal forest (Tiaga)

A

○ Freezing temperatures for 6 to 8 months
○ Characterised by coniferious forest
○ 16 million km2
○ 11.5% of terrestrial ecosystem area
○ Low tree species diversity
○ Sequesters about 20% of global carbon (not as much as expected for its area)

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2
Q

What trees are boreal forest characterized by?

A

Coniferous forest

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3
Q

Does boreal forest sequester the amount of carbon expected for its area?

A

No - only 20% of global carbon, more is expected

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4
Q

Artic Tundra

A
  • Tundra = treeless
    • Lands beyond northern tree limit
    • 7.5 million km2
    • 5.5% of terrestrial land surface
    • Greater than 0 degrees only 2-6 months of the year
    • Grasses and sedges , or shrubs dominate
    • Majority is snow covered
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5
Q

High Artic

A
  • Features very little grasses, sedges and shrubs
    • Light doesn’t limit productivity due to 2 hour days
    • Slow nutrient cycling and cold conditions determine productivity
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6
Q

Artic and Boreal ecosystems commonalities

A

Environmental commonalities:

  • Cold
  • Short growing season (summer)
  • Long snow cover duration
  • Permafrost
  • High winds, ice abrasion

Ecology commonalities

  • Slow decomposition
    -Low nutrients
  • Freeze tolerant plants
  • Low biodiversity
  • Slow growth
  • Great longevity
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7
Q

GPP

A

-Plants take up carbon by photosynthesis
-Ecosystem measure

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8
Q

NPP

A

-Losses of CO2 due to respiration
- Photosynthesis - respiration
- GPP- NPP
-Associated with growth

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9
Q

Ecosystem respiration R eco

A
  • Plant respiration and soil respiration
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10
Q

NEP/NEE

A
  • Overall uptake of carbon for the system
    - Carbon balance
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11
Q

Net biome production

A

-Considers many years
-Whole biome area
- Net balance is easily switched between source and sink

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12
Q

High latitude ecosystem NPP

A
  • Based on an equal area basis
    • Boreal forest has a poor NPP

-Once carbon is taken up it stays in Boreal forest for long time periods

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13
Q

Carbon density

A
  • Same in boreal forests as tropical forest despite a much smaller NPP
  • Tundra has large carbon density
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14
Q

How much more carbon is there in soil than plant biomass in boreal forest?

A

2-3 times more

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15
Q

How much more carbon is there in soil than plant biomass in tundra?

A

5 times

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16
Q

Carbon turnover rates between tundra, boreal forest and tropical forest

A
  • Carbon taken up to then be release again
    • Tundra takes 65 years for turnover
    • Boreal forest takes 53 years
  • Tropical forest take 14.2 years
17
Q

Changing high latitude C

A

-Growing season summed NDVI = greenness over time (season length)

- Excellent proxy for productivity (biomass production and gross carbon gain)
  • High latitude ecosystems are greening-Biomass is increasing = more carbon gain in plants

-Boreal and arctic is increasing its productivity

  • NPP is therefore increasing
18
Q

Boreal Treeline advance

A
  • Boreal trees advancing onto tundra

-Extent to this globally evidence is unclear

19
Q

Alaska

A
  • Younger trees
    -No older trees advancing into tundra
    • Younger system on forest tundra transition
20
Q

Tundra shrubification

A
  • Increase in shrub abundance
    • 28% hiltops to 160% floodplains
    • NPP increasing
  • Models predict increased C in more biomass = greater removal of CO2 from the atmosphere

-But more C in soil than biomass in high latitude ecosystems

-Hartley et al. (2012): C stocks and C fluxes in adjacent forest and tundra

21
Q

Will artic and boreal forest become a greater carbon sink?

A
  • Plants will, but soil processes may combat this
    • Models predict increased C in more biomass = greater removal of CO2 from the atmosphere
    • But more C in soil than biomass in high latitude ecosystems
    • Far less carbon in birch forest soil than tundra
    • Birch may be more productive in terms of plant biomass but has half the carbon
    • Boreal forest has ⅔ carbon stored compared to tundra
      • As boreal forest moves on to tundra it may cause carbon release
22
Q

Biomass increase vs soil decomposition

A
  • Priming of decomposition
    • Stimulate decomposition
    • NEE could end up releasing carbon
    • Tree planting is not a simple a process as previously thought
23
Q

The future? Model projections for arctic and boreal regions

A
  • Models represent increases in soil- warming respiration losses of C
    • But priming not properly represented
    • Vegetation carbon will increase
    • Ecosystem carbon storage shall increase over time
    • Runaway climate change will result in lots of co2 release due to warming soils and decomposition
      ○ Tundra shrubification due to warmer temperatures
    • Greater CO2 means more growth for plants however, but less carbon in these than soil in tundra
24
Q

The main issue with artic greening and productivity

A

-Increase C storage might not occur if greater photosynthesis/growth does not compensate for greater respiration (due to warming or priming).

  • So, high latitude ecosystems ‘could’ become a source of C
  • Greater photosynthesis must compensate for greater respiration to to priming/warming.