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Ice-albedo feedback
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Ice-albedo feedback (or snow-albedo feedback) is a climate feedback process where a change in the area of snow-covered land, ice caps, glaciers and sea ice alters the albedo. As a result of these albedo changes, changes to energy balance occurs, acting to reinforce the original change which caused the initial alteration in ice area. Cooling tends to increase ice cover, which in turn creates more cooling. During warming, the reverse is true, as melting reduces ice cover.

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Encyclopedia
Ice-albedo feedback (or snow-albedo feedback) is a climate feedback process where a change in the area of snow-covered land, ice caps, glaciers and sea ice alters the albedo. As a result of these albedo changes, changes to energy balance occurs, acting to reinforce the original change which caused the initial alteration in ice area. Cooling tends to increase ice cover, which in turn creates more cooling. During warming, the reverse is true, as melting reduces ice cover.
The effect also applies on the small scale to snow-covered surfaces. A small amount of smow melt exposes darker ground which absorbs more radiation, leading to more snowmelt.
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