L5 - Feedbacks Flashcards

1
Q

What does an initial change in radiative forcing induce changes in? (clear sky feedback)

A
  • Water vapour in atmosphere
  • Vertical distribution of water vapour
  • Tropospheric lapse rate (in cloud free regions)
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2
Q

Emissivity

A

the ratio of radiation of an object to that of a blackbody at the same temperature

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3
Q

negative lapse rate feedback?

A

larger temp change in the upper troposphere

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4
Q

positive lapse rate feedback?

A

larger temperature change at the surface

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5
Q

Where is global warming strongest?

A

Warming is amplified at the poles (2-6 times stronger) due to snow albedo feedback and increase in lapse rate (positive LR feedback)

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6
Q

What is the impact of doubling co2 on lapse rate at the equator?

A

This will result in a negative lapse rate feedback with a larger temp change in upper troposphere. This is because there is more water vapour in the atmosphere and higher up, increasing temps here. However at the equator there is some evaporative cooling due to more rainfall

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7
Q

What is the impact of doubling co2 on lapse rate at the poles?

A

A positive lapse rate feedback will result with a larger temperature change at the surface than in the upper troposphere. This is because increasing co2 increases ice melting thus lowers albedo and more absorption takes place at the surface, however there is little change higher up.

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8
Q

Temperature gradient (Teq - Tp):

A

Lower troposphere -> negative trend
Upper troposphere -> positive trend

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9
Q

Positive ice albedo

A

cooling amplified by LW radiation reflected

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10
Q

Negative-growth-thickness feedback

A

increased heat loss from ocean when ice melts, more ice production, original thinning will be less

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11
Q

Cirrus clouds

A

high thin clouds with a LOW albedo. Tend to warm. Long wave term dominant

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12
Q

Cumulus clouds

A

low thick clouds with HIGH albedo. Tend to cool. Short wave albedo term dominant

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13
Q

Rubisco

A

primary carboxylase of the photosynthetic process.
- Binding to O2 = respiration
- Binding to CO2 = photosynthesis

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14
Q

Chloroplasts

A

specialized cell organelles which are located in mesophyll and palisade cells in leaves

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15
Q

Law of diminishing returns

A

when you increase the limiting factor (co2), the short term plant response will likely saturate

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16
Q

Permafrost/cryotic soil

A

soil which is at or below 0 degrees for 2 or more years
- Little decomposition
- When they thaw large amounts of methane are released

17
Q

how does forest cover impact albedo

A

decreases albedo by absorbing LW radiation

18
Q

components of radiative forcing?

A

blackbody feedback (0), lapse rate feedback (L), water vapour feedback (W), cloud feedback (C), albedo feedback (a)

19
Q

How do clouds heat?

A

By trapping LW radiation with high cirrus clouds. These have low albedo and let most SW radiation through

20
Q

How do clouds cool?

A

By reflecting SW radiation with low cumulus clouds. These have high albedo

21
Q

What are the carbon and biogeochemical feedbacks?

A
  1. Concentration carbon
  2. Climate carbon
  3. Permafrost
    4.Interactions climate and terrestrial biosphere
22
Q

What is the effect of increased co2 on stomata size over time?

A

Decreases stomata size, thus less water loss. Extended growing season in water limited environments and reduction in soil drying.

23
Q

What limits plant production?

A

Temperature, radiation and water supply