ECEC - arctic ecosystems Flashcards

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1
Q

describe polar amplification

A
  • snow and ice melt revealing more dark surfaces which absorb heat
  • Positive feedback loop
  • Lack of plants in the arctic – reduced evapotranspiration – this is a cooling mechanism – more heat goes into warming instead of cooling process - the atmospheric layer that has to warm in order to warm the surface is shallower in the arctic
  • as sea ice melts, solar heat is absorbed by the oceans is more easily transferred to the atmosphere
  • alterations in atmospheric and oceanic circulation can increase warming
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2
Q

describe permafrost

A

permanently frozen ground (at-least 2 consecutive years) which stores carbon as peat and methane - more than twice as much carbon than the atmosphere - stores organic soil carbon

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3
Q

what can melting of permafrost cause?

A

sunken and misshapen grounds when ice melts, trees falling over from melt = ‘drunken forest’

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4
Q

why is warming concentrated in the arctic?

A

because it is greatest in high northern latitudes

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5
Q

describe the positive feedback of permafrost thaw

A
  • At first plants are able to get more nutrients and water helping them to aid growth
  • Therefore initial stage of thaw can cause increase of co2 uptake
  • Over time overall there is more carbon being released than taken in
  • As lower ground gets saturated with water a wetland could be created and more methane is released
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6
Q

what is done to help reduce the effects of permafrost thaw?

A
  • Roads must be kept clear of snow in winter to allow permafrost to get really cold and reduce effects of heating of the dark surfaces during the summer
  • Heat exchangers can also be used to remove heat from land and keep permafrost as cold as possible to avoid slumping
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7
Q

when is snow cover loss fastest?

A

spring/ early summer

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8
Q

what is a growing season?

A

snow free period - 2 weeks longer now than it used to be

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9
Q

what is the consequence of the now 2 week longer growing season?

A

increase in tundra ecosystem productivity and respiration

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10
Q

what is arctic greening and its consequence?

A

increased plant growth of more productive plants -Increase in carbon sequestered by greening tundra

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11
Q

what is the consequence of loss of arctic sea ice and the timing of melting?

A
  • more heat absorbed by Earth’s surface
  • Big consequence is loss of shiny surface and exposed ocean to absorb heat
  • Big effects on marine ecosystem
  • Changes in time of melt and freeze each year impacts timing of food availability
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12
Q

what are the ecological consequences of sea ice decline?

A
  • Affects availability of ice-associated zooplankton and forage fish (critically important for sea birds, marine mammals and fish species)
  • Sub-arctic species are expanding northward to where it is colder which then compete with the arctic species – puts pressure on them for lack of resources and competing for the same niches
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13
Q

what are the ecological consequences of sea ice melting for pinnipeds?

A

Pack ice breeding seals will experience reproductive failure more frequently – late winter/ early spring breeding habitat becoming less stable

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14
Q

what is the effect of sea ice reduction on polar bears?

A
  • Reduced seals effects polar bear populations – shift in trophic interactions
  • As sea ice thin – more fractured and labile so polar bears need to swim more and use more energy – lack of food to support this – reduced fat reserves to defend from the arctic temperatures
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15
Q

how much of the land in the northern hemisphere is permafrost?

A

24%

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16
Q

what are the predicted affects on sea ice if global warming stays below 1.5 degrees or reaches 2 degrees?

A

1/100,000 (exceptionally unlikely) for an ice-free Arctic if global warming stays below 1.5 °C
But 1/3 (39%) chance of ice free if global warming is limited to 2.0 °C