Linked from

The 39 pages that link to Albedo, each with the reason it gives.

• Radiative forcingRelated: Albedo changes alter how much solar energy Earth absorbs.

• Rayleigh scatteringRelated: Scattering by atmospheres and particles helps determine how much radiation is reflected.

• ReforestationRelated: Dark forests can absorb more sunlight than the open land they replace, affecting local climate.

• Solar irradianceRelated: Together with irradiance, albedo determines how much solar energy a surface absorbs.

• ClimateRelated: Changes in snow, ice, clouds, or land cover alter how much solar energy Earth absorbs.

• SeasonsRelated: Snow and ice reflect sunlight, reinforcing seasonal cooling in some regions.

• AfforestationRelated: Darker tree cover can reduce surface reflectivity and partly offset climate cooling.

• MicroclimateRelated: Differences in surface reflectivity change how much solar energy a place absorbs.

• Greenland ice sheetRelated: Snow and clean ice reflect sunlight, while darker surfaces absorb more energy and melt faster.

• SnowmeltRelated: Fresh, bright snow reflects much sunlight, while darker or dirty snow absorbs more energy.

• IceRelated: Bright ice reflects sunlight and helps regulate how much energy Earth absorbs.

• SnowpackRelated: Bright snow reflects much sunlight, while darkening increases absorbed energy and can speed melt.

• Ice ageRelated: Expanding bright ice reflects sunlight and reinforces cooling, while retreating ice weakens that feedback.

• Climate of the ArcticRelated: Bright snow and ice reflect sunlight, while darker ocean absorbs more energy.

• GlaciationRelated: Bright snow and ice reflect sunlight, reinforcing cooling and ice growth.

• Faint young Sun paradoxRelated: A darker early Earth would have absorbed more sunlight despite the Sun’s lower luminosity.

• Polar climateRelated: Snow and ice reflect much sunlight, limiting surface warming.

• Climate change and forestsRelated: Forests can absorb more sunlight than snow-covered land, complicating their cooling effect.

• James LovelockRelated: Daisyworld’s contrasting daisies change planetary albedo and thereby influence temperature.

• Huronian glaciationRelated: Expanding ice reflects more sunlight, creating a positive feedback that can intensify cooling.

• Reflection nebulaRelated: Dust albedo helps set how much nearby starlight can emerge as scattered light.

• Sturtian glaciationRelated: Expanding ice increased reflectivity, reinforcing cooling as glaciation spread.

• SunlightRelated: Albedo determines how much incoming sunlight warms a surface.

• HaptophyteRelated: Coccolithophore blooms can increase ocean-surface reflectance through suspended calcite plates.

• Marinoan glaciationRelated: Expanding ice raised planetary reflectivity, reinforcing cooling in Snowball Earth models.

• Earth’s shadowRelated: The Moon’s reflectivity affects how bright it appears against Earth’s dark shadow.

• Black (color)Related: Low visible-light albedo is characteristic of surfaces perceived as black.

• Deforestation and climate changeRelated: Forest removal changes surface reflectivity, which can partly offset or amplify local warming.

• Mikhail BudykoRelated: Snow and ice reflect sunlight, linking Budyko’s heat balance to powerful climate feedback.