
Arctic Climate Change Impacts
Interactive Video
•
Science, Geography
•
9th - 12th Grade
•
Hard

Jackson Turner
FREE Resource
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10 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Why is the Arctic often referred to as the 'canary in the coal mine' for climate change?
Because it is a major source of fossil fuels.
Due to its role in global ocean currents.
Because it is highly sensitive to climate changes.
Due to its large population of polar bears.
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What happens when the Arctic warms slightly?
More snow and ice form, increasing reflectivity.
Snow and ice melt, exposing darker surfaces.
The Arctic becomes more reflective.
The Arctic cools down rapidly.
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How does Arctic sea ice contribute to insulation feedback?
By increasing the Earth's albedo.
By acting as a barrier between cold air and warm water.
By releasing heat into the atmosphere.
By absorbing more sunlight.
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is a negative feedback loop in the context of the Arctic?
A loop that only occurs in winter.
A feedback that always leads to cooling.
A process that stabilizes the system by counteracting changes.
A process that amplifies initial changes.
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How do clouds formed from melting ice affect the Arctic climate?
They always cool the atmosphere.
They permanently increase reflectivity.
They have no effect on the climate.
They can initially cool but later warm the atmosphere.
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the effect of positive feedback loops on the Arctic climate?
They always result in cooling.
They have no significant impact.
They lead to larger deviations from equilibrium.
They stabilize the climate.
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How does the warming of the North Pole compare to the equator?
The equator warms faster than the North Pole.
The North Pole warms at a slower rate.
Both regions warm at the same rate.
The North Pole warms at a faster rate.
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