Surface Albedo Modification (Technology Briefing)

Forest clearance in Boreal areas would mean more reflective snow – but less forest! (Derrick Midwinter/Flickr)

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Surface Albedo Modification is a theoretical solar geoengineering technique that aims to reflect more sunlight back to space by enhancing earth albedo – the sunlight reflected off the Earth’s surface. Proposals span a wide range – from growing crops that reflect more light, to the clearing of boreal forest in snowcovered areas; from covering large desert or ice areas with reflective materials to whitening mountaintops and roofs with white paint – all with a common goal: to increase the earth’s surface albedo.

Albedo describes how much solar radiation is reflected by a surface. A high albedo means most solar radiation is reflected, for example polar ice sheets. A surface with a low albedo, for example a dark ocean surface, reflects only a relatively small share and absorbs most of the solar radiation in the form of heat, thus contributing to warming the surrounding area.

Creating large surfaces with a higher albedo could increase the amount of solar radiation reflected from the Earth’s surface and could theoretically reduce the temperature of the atmosphere, because surfaces absorb less solar energy. However, the proposal would not reduce the concentration of greenhouse gases in the atmosphere, which would continue increasing. In most cases, the unwanted side effects on the ecosystems, fauna and flora, as well and human communities that depend on those ecosystems could be devastating.

The following outlines different approaches to modify surface albedo, mentions relevant actors involved and describes potential impacts.


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