CIP session 2: Climate Scenarios and Risk Flashcards

1
Q

Feedback mechanisms that amplify global warming

A

Uncertainty in feedbacks is the prime reason for uncertainty in future global mean temperature projections.
Water vapor feedback
ice-albedo feedback
cloud feedback

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2
Q

Essence of Climate models (how are they “made”)

A

based on conservation laws. There is discretization in space (boxes) and time (timesteps). What leaves one box must enter the other.

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3
Q

Why is resolution important?

A

Any subgrid process (i.e. a process operating at smaller temporal or spatial scale) cannot be resolved. It needs to be parameterized. This may cause uncertainty. (e.g. tropical cyclones are small and cannot be resolved by most climate models)

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4
Q

Emergent properties

A

large-scale features of climate systems naturally emerge (e.g. trade winds and jet streams)

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5
Q

Cloud feedbacks/ uncertainty reason

A

clouds affect many parts of the climate system (radiation, wind patterns and temperature distribution). They happen at a micro-scale and cannot be resolved

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6
Q

simple phyiscal drivers of extreme weather

A

-Shift in mean to warmer values will increase the frequency of heat extremes
-Warmer air can hold more water vapor (7% per 1 degree). There also more water in the air, means more water can fall down so more precipitation

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7
Q

complex physical drivers of extreme weather

A

Changes to the atmopsheric circulation can strongly affect extreme weather. When temperature differences become smaller, jet streams become weaker.

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8
Q

Physical drivers of increases in heatwaves

A
  • Global climate shift towards higher temperatres, causes higher probability of hot weather.
  • Due to slowe jet streams high pressure areas get stuck, leading to longer heatwaves.
  • Heatwaves strenthen during drought because less evaporative cooling.
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9
Q

How does global warming cause more extreme rainfall?

A

Wamer air can hold more water (Clausius-Clapperon equation).

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10
Q

How does global warming affect hurricanes?

A
  • Hurricanaes become wetter due to incresed water holding capacity of air.
  • More ocean with 26+ T, hurricanes can extract more energy.
  • Slowed jet streams allow for hurricanes to stay in one place longer.
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11
Q

Tipping point (description)

A

A critical threshold at which the future state of a system can be qualitatively altered by a small change in forcing.

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