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loopster loopster
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7 years ago
Warming temperatures melt ice cover, exposing a darker surface that absorbs more solar radiation. In response, the air warms even further. This is an example of:
A) a stable-feedback mechanism.
B) a negative feedback mechanism.
C) a positive feedback mechanism.
D) a variable-feedback mechanism.
Textbook 
Atmosphere: An Introduction to Meteorology

Atmosphere: An Introduction to Meteorology


Edition: 12th
Authors:
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eaudieaudi
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7 years ago
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loopster Author
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7 years ago
Didn't expect that to be the answer... Thank you for being right all the time lol
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