Lecture 8: Contrasting impacts of extreme events & trend CC on Arctic ecosystems Flashcards

1
Q

Arctic is warming, some regions __ DC warmer than in 1950’s

A

2-3 degrees C

  • due to polar amplification
  • poles warm more than rest of world
    • arctic +0.09 DC / decade
    • global av +0.06 DC/ decade
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2
Q

polar amplification -

A

greater warming a the poles

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3
Q

warming effect on terrestrial ecosystems =

A
  • snow is melting earlier
  • longer snow free period
  • longer growing season
    • = arctic greening as plants have longer to establish & warmer temperature
    • looking at NDVI satellite images you can see greener land
  • – longer growing season or bigger plants
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4
Q

“greening” of the arctic: shrubs

A
  • shrubification

increase in shrub abundance 28% on hilltops to 160% floodplains between 1950 -2000

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5
Q

Arctic “shrubification” alters

A
  • photosynthesis
  • priming of soil C decomposition
  • influence permafrost thaw
  • alter surface energy balance (transpiration/albedo)

– carbon balance unknown, C into ground. microbes respire, release etc

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6
Q

arctic warming = more intense in summer/winter

A

more in winter than summer

- with more extreme climatic events

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7
Q

extreme winter events:

A

1) extreme winter warming
2) frost-drought
3) icing

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8
Q

Extreme winter warming

A
  • e.g. Dec 2007 North-west Scandinavia
  • max temp 4-12 DC for 5-12days
  • ground surveys: 50% loss live biomass
  • 26% reduction in NDVI
  • – warming causes bud to burst (plants think its spring) & lose their freeze tolerance
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9
Q

frost-drought

A
  • less snow so plants aren’t protected
  • winter solar radiation on canopies but soil frozen -
  • plants try to transpire BUT roots are frozen
  • desiccation damage
  • evergreen shrubs particularly vulnerable
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10
Q

icing

A
  • rain on snow (refreezing) & winter warming
  • ice encasement of vegetation
  • High CO2 or hypoxia, AS encasing stops gas exchange BUT questionable –> (Preece et al 2012 & 2013)
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11
Q

arctic browning & biotic drivers

A

Frost drought
icing
extreme winter warming BUT OTHER THINGS TO
- biotic drivers accelerate browning
- maritime & warmer arctic may be early warming
– arctic browning now becoming an issue

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12
Q

things that make arctic brown

A

frost drought
icing
extreme winter warming

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13
Q

things that make arctic green

A
  • warming

- shrubification

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14
Q

arctic green/ brown

A

in 2015, 4 years browning trend (2010-2014)

  • recent return to greening overall, but major uncertainty
  • all models predict greening!!
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15
Q

where are we heading? (arctic environment)

A
  • -> trends dominate, = greening!! with some browning episodes
  • events dominate = browning will occur!
    • hard to predict
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16
Q

trends =

A

greening

17
Q

events =

A

browning

- events are sporadic, temporary (recover), hard to predict, and hard to monitor

18
Q

extreme events in wine are ___ in frequency

A

increasing

19
Q

extreme events caused

A

widespread plant mortality, often to dominant species

– have major impacts on community structure & C balance