56: Climate Models and Predictions Flashcards

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1
Q

Can we just extrapolate (extend) the Keeling Curve?

A

No! there are other greenhouse gases whose concentrations are changing, and the ocean will remain warm for a while

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2
Q

What is a positive feedback mechanism?

A

reinforces and amplifies the ongoing trend

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3
Q

What is an example of a positive feedback mechanism?

A

higher temperature –> more water evaporation –> more water vapor in the atmosphere –> water vapor is a greenhouse gas –> higher temperature

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4
Q

What is a negative feedback mechanism?

A

diminishes or reverses a particular trend and maintains the initial conditions, goes against the change

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5
Q

What is an example of a negative feedback mechanism?

A

higher temperature –> more water evaporation –> more water vapor in the atmosphere –> more clouds –> more reflection of sunlight –> less sunlight reaching the surface –> lower temperatures (cooling)

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6
Q

What are climate models?

A

are computational devices for solving large sets of equations
- not perfect, but they can be tested against reality over time

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7
Q

what can climate models create?

A

possible scenarios, some more optimistic than others
(doesn’t mean everything is possible, not all answers are good answers but there are several answers that are possible)

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8
Q

In context of climate, what are scenarios called?

A

representative concentration pathways (RPC)

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9
Q

What are climate scenarios now?

A
  1. high emission scenario: no climate policies (global temperature increases 4.1-4.8C)
  2. mid-range emission scenario: current policies (global temperatures increase 2.5-2.9C)
  3. low emission scenario: global temperature increases 1.5 C
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10
Q

What is a tipping point?

A

critical point in a situation beyond which a significant and often unstoppable effect or change takes place

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11
Q

What does spurious mean?

A

not being what it purports to be; false or fake

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