Carbon Cycling at High Latitudes Flashcards

1
Q

What are the main land covers of high latitudes?

A

Boreal forests: coniferous, freezing temps for 6-8 months
Arctic tundra: treeless, beyond northern tree limit. Grasses, sedges and shrubs.

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2
Q

What are characteristics of high latitude ecosystems?

A
  • Cold, so slow decomposition
  • Short growing season, low nutrients
  • Snow cover, freezing tolerance
  • Store lots of carbon underground
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3
Q

What is NPP?

A

Net primary productivity
NPP = GPP - R

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4
Q

What is NEP?

A

Net ecosystem productivity
NEP = NPP - Reco

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5
Q

How much carbon do boreal forests store in soil?

A

2-3 times more C in soil than in biomass

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6
Q

How much carbon does tundra store in soil?

A

5 times more C in soil than in biomass

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7
Q

Is the turnover time short or long for high latitude ecosystems?

A

highest turnover time, keep molecule of carbon in ecosystem for the longest until it is released.

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8
Q

What has changed about the growing season in high latitudes and how do we know?

A

NDVI shows growing season in longer, meaning productivity is going up and there is more carbon gain in plants.

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9
Q

What is happening to the boreal treeline?
How do we know?

A

It is advancing onto tundra (northward)
There are more young trees at the edge of the tree line and more seedlings.

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10
Q

How much shrubification has there been on the hill tops?

A

Abundance has increased by 28% on the hilltops.

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11
Q

What do models predict about soil decomposition?

A

If there is more C in biomass, there will be more C removal from the atmosphere, meaning more C is in the soil. However this could cause priming of decomposition and carbon loss.

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12
Q

What is priming of decomposition?

A

Input of new carbon into the soil stimulates decomposition of old soil carbon.

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13
Q

What is a trade off to do with warming of high latitudes?

A

Warming will also increase respiration and soil respiration, meaning soil C storage might not increase.

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