A “Tragedy of the Commons” requires both a “tragedy” and a “commons.” What does the tragedy consist of in a system that is governed by the “Tragedy of the Commons” model?
1 point
An inevitable degradation
A region, such as a fishery or pasture
A possible degradation
The necessity of government regulation
2.[Q#3006]
A “Tragedy of the Commons” is most associated with:
1 point
Overuse of a resource
A fair allocation of resources
Un unfair allocation of resources
A small resource
Underuse of a resource
A large resource
3.[Q#3007]
Fisheries are observed to experience the “Tragedy of the Commons” when they:
1 point
Are unregulated and not shared
Are overregulated and shared
Are unregulated and shared
Have some large fishing vessels
Have many small fishing vessels
4.[Q#3009]
Fisheries are often described as being afflicted by “the Tragedy of the Commons.” Which of the following statements is true from this description of the situation?
1 point
Increases in technology mean that fishermen are no longer limited to sustainable fishing techniques.
Fisherman are forced to sell their catch at below market rates.
Fisheries are collective resources not owned by any one corporation or individual.
Both recreational and commercial fishermen use the resource.
Fishermen are forced to sell their catch at market rates.
5.[Q#3013]
To conserve the Alaska pollock fishery, the US government brought in permitting requirements, limited the number of allowed fishermen, imposed quotas, and even closed areas to fishing. Why did the government do this?
1 point
It was an attempt to deal with a “Tragedy of the Commons” problem.
It was an application of “NIMBY” to fisheries management.
It was an application of neo-Malthusian principles.
It was an application of the “precautionary principle” to fisheries management.
It was an attempt to apply a “Pigovian tax” to pollock fishermen.
6.[Q#3015]
Why can common use of a resource result in destruction of that resource?
1 point
Independent individuals disagree on the best long-term outcome.
Few people act rationally.
Individuals do not care about resources.
Group incentive is to exploit the resource beyond its carrying capacity.
Individual incentive may not be consistent with the group incentive.
7.[Q#3016]
Many places had common resources that’s uses were shared but did not deplete these resources. This is because the local people employed the following approach to avoid commons degradation:
1 point
Government regulation
Internal governance
External governance
Property rights/”Laissez-faire”
Personal action
8.[Q#3019]
Why is the “commons” part of the “Tragedy of the Commons” term potentially a poor name?
1 point
Fisheries are not “commons.”
The original commons were sustainably managed.
Tragedies are not inevitable.
The original commons were heavily regulated by government.
Few commons exist.
9.[Q#3021]
A property rights approach is having trouble dealing with some important “Tragedy of the Commons” issues. One of these is atmospheric pollution and climate change. Why might a property rights approach, in particular, be failing to curb the problem?
1 point
Lack of social community
Unclear group commons incentive
No commons ownership possible
Lack of individual incentive
Lack of enforcement
10.[Q#4052]
So far, the global average temperature of the 21st century has been higher than that of the 19th century. True or false?
1 point
True
False
11.[Q#4002]
Can you use weather data to determine the climate? Why?
1 point
Maybe – if the weather data is observational and not instrumental.
Yes – if you have enough weather records.
No – you can determine weather from climate, not the other way around.
Yes – climate and weather are approximately the same thing.
No – weather and climate are unrelated.
12.[Q#4005]
If the Earth is in “energy balance,” this means:
1 point
The incoming energy equals the outgoing energy.
Different parts of the Earth have (almost) the same energy.
Western countries produce as much energy as they use.
Only sustainable sources of energy are employed.
The greenhouse effect is not operating.
13.[Q#4011]
Near the end of the Cretaceous period, about 65 million years ago, the Earth was much warmer than it is today. Scientists ascribe this, in part, to:
1 point
High CO2 concentrations
The different fauna that existed
The higher sea levels that were prevalent
The existence of the dinosaurs
The impact of a large asteroid or comet
14.[Q#4019]
Over the past 800,000 years, when was carbon dioxide in the atmosphere the highest?
1 point
Around 800,000 years ago
Today
At the peak of the last glacial period, about 10,000 years ago
Around 1850
At the peak of the last interglacial period, about 100,000 years ago
15.[Q#4022]
Which of the following data sources informs us that the Earth’s climate was once in a glacial period?
1 point
Satellite data
Ice cores
Anemometers
Tide gauges
St. Matthews Island reindeer population counts
16.[Q#4026]
According to proxy and instrumental data, what is the general trend of global temperature in the last 200 years?
1 point
3 to 5 degrees Fahrenheit warming
A clear set of cycles based on orbital forcing (Milankovitch cycles)
A series of 11-year cycles based on volcanic activity
Between -1 and 1 degree Fahrenheit cooling or warming
1 to 2 degrees Fahrenheit warming
17.[Q#4030]
If there was no atmosphere, the Earth’s average temperature would be about -18 degrees Celsius (which is below 0 degrees Fahrenheit). The Earth is much warmer than this! Why?
1 point
The sunspot cycle is currently warming the Earth.
Human emissions of carbon dioxide have vastly increased the Earth’s temperature.
The Earth’s atmosphere traps heat like a natural greenhouse.
The Sun has become much hotter over geological time.
Periodic volcanic eruptions put soot in the Earth’s atmosphere, warming the Earth.
18.[Q#4033]
Why is carbon dioxide (CO2) thought to act as a “greenhouse gas”?
1 point
CO2 is more transparent to visible than to infrared radiation.
CO2 is largely transparent to infrared radiation.
CO2 is denser than oxygen, and so acts as a blanket on the surface of the Earth.
CO2 is less dense than nitrogen, and so shields the top of the atmosphere from the Sun’s rays (insolation).
CO2 is relatively viscous, reducing atmospheric convection.
19.[Q#4034]
How might a change in albedo, caused by increased forest cover, warm the Earth?
1 point
Forests replace deserts, which absorb large amounts of CO2.
Forests are darker than grasslands.
Increased forest cover removes CO2 from the atmosphere.
Forests reduce the climate differences between the oceans and the land.
Forests increase precipitation, which can encourage the growth of ice sheets.
20.[Q#4038]
What physical feature of the “stable isotopes” in water means that they vary with climate in ice cores, so they can tell us about changes in Earth’s temperature over time?
1 point
Lighter isotopes are negatively charged.
Heavier isotopes require more heat energy to evaporate.
Unstable isotopes decay, preferentially leaving stable isotopes, which do not.
Lighter isotopes have higher albedos, decreasing the surface temperature.
Heavier isotopes sink to the bottom of ice cores.
21.[Q#4040]
How might both ice sheets and vegetation change the climate?
1 point
Both ice sheets and vegetation continually suck heat out of the atmosphere.
Both ice sheets and vegetation change the albedo of the Earth’s surface, altering the amount of sunlight that is reflected.
Both ice sheets and vegetation increase the amount of water in the oceans, allowing more carbon dioxide to be dissolved there.
Both ice sheets and vegetation continually remove water from the atmosphere.
Both ice sheets and vegetation contribute carbon dioxide to the atmosphere, creating a natural greenhouse effect.
22.[Q#4041]
In what situation is instrumental data preferable to proxy data?
1 point
Observing the Milankovitch cycle
Detecting evidence of the “snowball Earth”
Developing a millennia-long record of temperature
Knowing the precision of current temperature
23.[Q#4043]
Why are sea levels projected to further increase over the next century?
1 point
Rising temperatures of the oceans will result in thermal expansion of the water.
Rising temperatures of the atmosphere will increase the amount of glacial meltwater being added to the oceans.
Rising sea levels are not projected to increase measurably until after 2100.
Rising temperatures of the oceans will result in thermal expansion of the water, and rising temperatures of the atmosphere will increase the amount of glacial meltwater being added to the oceans.
None of the other options is correct.
24.[Q#4045]
If Earth had no atmosphere, its average temperature would:
1 point
Not change
Be more like that of the Moon
Behave unpredictably
Increase in response to the change in insolation
Be more like that of Venus
25.[Q#4046]
Venus is closer to the Sun than the Earth and its Moon. If Venus and the Moon had the same atmosphere (be it thick or thin) and roughly the same albedo, we could confidently predict that:
1 point
The Earth, Moon, and Venus would have close to the same average surface temperature.
The Earth would not be cooler than the Moon.
The Earth would be the same temperature as, or warmer than, the Moon.
Venus would be warmer than the Moon.
Venus would be cooler than the Moon.
26.[Q#4050]
Earth’s climate has recently been linked to the Milankovitch cycle. If this natural trend were to continue, we would expect that the average temperature of the Earth will do what over the next 10,000 years?
1 point
Decrease slowly (by less than 5 degrees Fahrenheit)
Increase quickly (by at least 5 degrees Fahrenheit)
Decrease quickly (by at least 5 degrees Fahrenheit)
Increase slowly (by less than 5 degrees Fahrenheit)
Not measurably change
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