lecture 23- climate change model scenarios Flashcards

1
Q

What are the ranges of responses to environmental problems?

A

1- Doing nothing

2- Mitigation, or the action of reducing the severity or seriousness of a (environmental) problem.

3- Adaptation, or reducing our vulnerability to impacts by increasing our resilience or capacity to deal with them.

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2
Q

What are the consequences of the range of responses?

A

Adaptation, mitigation, and doing nothing are not mutually exclusive.
And each choice comes with consequences (refer to triangle in notes).

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3
Q

What is the challenge of scenarios?

A

Near an infinite number of possibilities; no way to know which is correct, and which could be reasonable.

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4
Q

Are scenarios predictions?

A

No. Scenarios allow investigations of the implications of various developments and actions (“what-if”),

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5
Q

What is the issue with scenarios that is specific to climate modeling?

A

Given the complicated nature of Earth system models, only a few scenarios can be properly evaluated, and every group must use similar scenarios to permit comparisons.

We must arbitrarily choose a few scenarios that simultaneously capture the range of possible futures while being meaningful and useful for planning.

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6
Q

How Do We Come Up With Scenarios?

A

A consensus must be established on a limited set of different enough scenarios to learn from those differences and estimate associated uncertainties; Requires lots of coordination, we need institutions to help us.

For coordinated efforts at an international level, this is generally taken care of by a dedicated organization: IPCC

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7
Q

What are the drivers of IPCC scenario-making?

A

1- Geophysical driving forces: GHG and aerosol emissions, land use, Earth system response;
- emissions will shape what will happen-what worsens climate change or things that help

2- Socio-economic driving forces: Population, technology, economic development, and associated energy needs and geophysical implications (emissions, land use, etc.);

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8
Q

What drives how we approach the problem?

A

1- Societal/policy drivers: emphasis on sustainability, regional rivalry, inequality, fossil fuel-intensive development…

2- Types of possible responses (e.g., mitigation, adaptation),
agreed-upon targets (e.g., “well below 2°C”)
- or you can temporarily forget about the future, and focus on a goal- collectively decide on a degree limit, but if we pass it what are the implications.

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9
Q

Explain the institutional IPCC context.

A

Need for a range of outcomes to grasp the many issues;

Working groups coordination: scientific basis, impacts, response.

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10
Q

What are the dominant IPCC Scenarios?

A

1) Create categories of scenarios (“socio-economic pathways”) rooted in challenges of different types of responses.

2) Complement with an associated radiative forcing by 2100.

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11
Q

What does it mean for the IPCC to be milestone-centric? Why do they do this?

A

For example, what will climate change look like when a particular threshold is reached, such as 2°C warming.

Likely reason: patterns look similar for all scenarios at a specific threshold; what changes for a given scenario is if or when that threshold is reached.

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12
Q

What are the predicted temperature changes?

A
  • More over land than over water;
  • More at high latitudes and in winter than at low latitudes or in summer;
  • More at night than during the day.
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13
Q

What are the predicted evaporation changes?

A

Evaporation increases; but patterns of precipitation change:

Contrast between wet and dry regions and seasons will generally increase (to a first order, dry regions get drier, wetter regions will get more precipitation).

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14
Q

What are predictions dependent on?

A

Overall predictions are very dependent on scenarios → We can change the outcome.

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15
Q

What is an example of change that will take longer?

A

Some changes are expected to proceed more slowly and last considerably longer, such as for sea levels.

Even in scenarios where air temperatures stop rising beyond a certain level (e.g., 1.5°C), the slow mixing and warming of the oceans should lead to significant sea-level rises in a 1000-10000 yr horizon.

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