Ice and snow albedo-temperature feedback: Difference between revisions

From Glossary of Meteorology
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|Meaning=A [[positive feedback]] mechanism involving ice and  [[snow cover]], [[surface albedo]], and [[temperature]].
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|Explanation=For example, given an initial warming, a decrease in snow and [[ice cover]] occurs, lowering the  surface albedo. This causes an increase in the [[absorption]] of [[solar radiation]], which amplifies the  initial increase in temperature.
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== ice and snow albedo&ndash;temperature feedback ==
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<div class="definition"><div class="short_definition">A [[positive feedback]] mechanism involving ice and  [[snow cover]], [[surface albedo]], and [[temperature]].</div><br/> <div class="paragraph">For example, given an initial warming, a decrease in snow and [[ice cover]] occurs, lowering the  surface albedo. This causes an increase in the [[absorption]] of [[solar radiation]], which amplifies the  initial increase in temperature.</div><br/> </div>
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Latest revision as of 10:23, 30 March 2024

A positive feedback mechanism involving ice and snow cover, surface albedo, and temperature.

For example, given an initial warming, a decrease in snow and ice cover occurs, lowering the surface albedo. This causes an increase in the absorption of solar radiation, which amplifies the initial increase in temperature.

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