Practice Flashcards

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1
Q

What is the IPCC?

A

Intergovernmental Panel On Climate Change

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2
Q

What is the approximate global average surface temperature?

A

15 degrees celcius

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3
Q

What is the definition of albedo?

A

The fraction of incoming sunlight that is reflected

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4
Q

What is global warming potential?

A

A measure of the relative potency of different gases

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5
Q

Sea level is currently…

A

rising globally at 3-4mm per year

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6
Q

What is the largest single source of uncertainty in predictions of global mean temperature change for the end of the 21st century?

A

Variations in future anthropogenic greenhouse gas emissions

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7
Q

What is a climate change scenario?

A

A description of a feasible future climate

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8
Q

What is a Complex Climate Model?

A

A mathematical representation of all the physical processes and feedbacks which affect the Earth’s climate

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9
Q

According to the IPCC AR6 model projections, what is the maximum likely sea level rise by 2100?

A

1m

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10
Q

Which of the following emissions are not part of an emission scenario?

A

Emissions of soot by cars

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11
Q

What is a regional climate model?

A

A model which covers a part of the world in more detail than a global climate model

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12
Q

Approximately, by how much is temperature likely to increase in Reading by 2050?

A

2-3 degrees celcius

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13
Q

How is average rainfall likely to change in southern England?

A

Less in the summer, more in the winter

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14
Q

The most recent decade has been approximately how much warmer than pre-industrial times?

A

1.5 degrees celcius

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15
Q

What is the long term temperature goal in the Paris Agreement?

A

To hold the increase in temperature to well below 2 degrees above
pre-industrial levels and pursue efforts to limit the increase to
1.5 degrees.

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16
Q

What is meant by the term CO2 equivalent?

A

It expresses the effect of a greenhouse gas in terms of the
amount of CO2 which would have the same effect

17
Q

What is climate feedback?

A

A response to a climate process that either intensifies or minimizes the initial effect of a climate forcing (often either warming or cooling)

18
Q

What is an example of a positive climate feedback?

A

The melting of polar ice, a drop in albedo with the melting of polar ice - particularly sea ice, the release of carbon as a result of melting permafrost, the amount of water in the atmosphere, this increases as the world gets warmer, and puts even more water into the atmosphere

19
Q

What is an example of a negative climate feedback?

A

Excess cloud formation from ocean evaporation, increasing temperature radiates more heat into space, this is called Planck feedback and comes from the Stefan-Boltzmann law

20
Q

What is climate forcing?

A

Climate forcing is the physical process of affecting the climate on the Earth through a number of forcing factors.

21
Q

What is an example of climate forcing?

A

Variations in solar radiation levels, volcanic eruptions, changing albedo, and changing levels of greenhouse gases in the atmosphere

22
Q

From what does the natural greenhouse effect occur?

A

Absorption of infrared radiation emitted by the Earth’s surface by water vapour and carbon dioxide

23
Q

Globally averaged surface temperatures in this decade have been…?

A

About 1.2 degrees Centigrade warmer the 1850-1900 average

24
Q

What is radiative forcing?

A

Radiative forcing is what happens when the amount of energy that enters the Earth’s atmosphere is different from the amount of energy that leaves it.
Radiative forcing is the imbalance in the planetary radiation balance caused by a climate change mechanism, and can be caused by both natural changes (e.g., changes in total solar irradiance) and human-induced effects (e.g., increased concentrations of greenhouse gases). When it is positive, the climate system tends to warm; when it is negative, the climate system tends to cool.

25
Q

What is total solar irradiance?

A

A measure of the solar power over all wavelengths per unit area incident on the Earth’s upper atmosphere. It is measured perpendicular to the incoming sunlight. TSI varies on a quasi-regular cycle about 11 years in length. Between the maximum and minimum of this solar cycle, the TSI varies by about ±1 W m^-2 or ±0.1%, leading to a radiative forcing of around 0.175 W m^-2.

26
Q

The human-induced greenhouse gas radiative forcing since pre-industrial times is due to…?

A

Carbon dioxide, methane, ozone, the halogenated gases and nitrous oxide.

27
Q

Calculations indicate that the central estimate of the surface warming induced by well-mixed greenhouse gases between the periods 1850-1900 and 2010-2019 was…?

A

…about 50% greater than the observed warming of 1 degree.

28
Q

If we emit a pulse of carbon dioxide into the atmosphere, approximately how much of it would remain in the atmosphere in 60 years time?

A

about 45%

29
Q

If the global-mean surface temperature rise due to human activity is (“to a 50% likelihood”) to be kept below 1.5 deg C, then what cumulative emission of CO2 (in Gigatonnes (Gt) CO2) is allowable, and approximately what proportion of this emission do we have left?

A

13%

30
Q

The global warming potential (GWP(100)) for an emission of nitrous oxide is almost 10 times higher than that of methane because…?

A