Linked from

The 28 pages that link to Ice–albedo feedback, each with the reason it gives.

• Arctic amplificationRelated: Declining sea ice and snow expose darker ocean and land, amplifying regional warming.

• AlbedoRelated: It is the clearest self-reinforcing climate effect driven by changing surface albedo.

• Milankovitch cyclesRelated: It amplifies modest orbital cooling into larger ice-sheet and temperature changes.

• Climate change in the ArcticRelated: Declining snow and sea ice intensify local warming by increasing absorbed sunlight.

• Climate sensitivityRelated: It contributes to sensitivity, especially in regions where snow and sea ice retreat.

• Snowball EarthRelated: Reflective ice could drive glaciation toward global coverage once cooling crossed a critical threshold.

• Arctic sea ice declineRelated: Retreating ice lowers reflectivity and increases absorbed solar energy.

• Pleistocene glaciationRelated: Reflective ice amplified the cooling that accompanied glacial expansion.

• Ice shelfRelated: Shelf breakup exposes darker ocean, changing local heat absorption.

• GlaciologyRelated: This feedback links melting ice to further warming and additional ice loss.

• Climate change in AntarcticaRelated: It amplifies surface warming where Antarctic snow and ice retreat.

• Last Glacial PeriodRelated: This feedback amplified cooling as ice sheets expanded and warming as they retreated.

• QuaternaryRelated: It amplified orbital cooling during Quaternary glacial expansions.

• Ice sheet dynamicsRelated: It links ice-sheet surface change with climate forcing, rather than describing ice flow mechanics.

• Glacial periodRelated: This amplifying loop helps small cooling shifts produce extensive glaciation.

• Quaternary glaciationRelated: It amplified cooling as ice sheets spread across high-latitude continents.

• InterglacialRelated: Retreating ice exposes darker surfaces that absorb more sunlight and reinforce warming.

• Antarctic glaciationRelated: Once ice spread, increased reflectivity amplified Antarctic cooling.

• Last InterglacialRelated: Shrinking ice sheets reduced reflectivity, reinforcing warming during the interval.

• Milutin MilankovićRelated: This feedback can amplify the modest orbital sunlight changes in Milanković’s calculations.

• Arctic ice packRelated: Shrinking ice cover lowers Arctic reflectivity and can amplify regional warming.

• Mikhail BudykoRelated: This feedback drives the ice-boundary instability in Budyko’s climate model.

• Polar regionsRelated: It can amplify warming as polar snow and ice retreat.