What are some examples of positive and negative climate feedback loops?

What will be an ideal response?


Answers will vary. An example of a positive feedback loop may be:
As air temperatures increase, evaporation increases. Warmer temperatures also increase the capacity to absorb water vapor. More water vapor in the atmosphere accelerates the greenhouse effect. As temperatures increase further, more water vapor can enter the atmosphere, causing temperatures to increase even more.
An example of a negative feedback loop may be:
As air temperatures increase, evaporation increases, leading to more condensation and cloud formation. Low, thick cloud cover increases the albedo of the atmosphere, thereby having a cooling effect on Earth.

Environmental & Atmospheric Sciences

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Define and discuss the range of a service, providing some original examples (i.e., examples NOT copied directly out of the textbook) to illustrate your points

What will be an ideal response?

Environmental & Atmospheric Sciences

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The diagram below depicts the



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B) carbon cycle.
C) titanium cycle.
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Environmental & Atmospheric Sciences

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