Matches in DBpedia 2014 for { <http://dbpedia.org/resource/Ice-albedo_feedback> ?p ?o. }
Showing items 1 to 25 of
25
with 100 items per page.
- Ice-albedo_feedback abstract "Ice-albedo feedback (or snow-albedo feedback) is a positive feedback climate process where a change in the area of snow-covered land, ice caps, glaciers or sea ice alters the albedo. This change in albedo acts to reinforce the initial alteration in ice area. Cooling tends to increase ice cover and hence the albedo, reducing the amount of solar energy absorbed and leading to more cooling. Conversely, warming tends to decrease ice cover and hence the albedo, increasing the amount of solar energy absorbed, leading to more warming.The effect also applies on the small scale to snow-covered surfaces. A small amount of snow melt exposes darker ground which absorbs more radiation, leading to more snowmelt.The effect has mostly been discussed in terms of the recent trend of declining Arctic sea ice.Internal feedback processes may also potentially occur, as land ice melts and causes eustatic sea level rise, and also potentially induces earthquakes as a result of isostatic rebound, which further acts to disrupt glaciers, ice shelves, etc.".
- Ice-albedo_feedback thumbnail Greenland_Albedo_Change.png?width=300.
- Ice-albedo_feedback wikiPageID "21435575".
- Ice-albedo_feedback wikiPageRevisionID "602340355".
- Ice-albedo_feedback hasPhotoCollection Ice-albedo_feedback.
- Ice-albedo_feedback subject Category:Climate.
- Ice-albedo_feedback subject Category:Climate_feedbacks.
- Ice-albedo_feedback type ClimateFeedbacks.
- Ice-albedo_feedback type Feedback113479380.
- Ice-albedo_feedback type NaturalProcess113518963.
- Ice-albedo_feedback type PhysicalEntity100001930.
- Ice-albedo_feedback type Process100029677.
- Ice-albedo_feedback comment "Ice-albedo feedback (or snow-albedo feedback) is a positive feedback climate process where a change in the area of snow-covered land, ice caps, glaciers or sea ice alters the albedo. This change in albedo acts to reinforce the initial alteration in ice area. Cooling tends to increase ice cover and hence the albedo, reducing the amount of solar energy absorbed and leading to more cooling.".
- Ice-albedo_feedback label "Eis-Albedo-Rückkopplung".
- Ice-albedo_feedback label "Ice-albedo feedback".
- Ice-albedo_feedback label "アイス・アルベド・フィードバック".
- Ice-albedo_feedback sameAs Eis-Albedo-Rückkopplung.
- Ice-albedo_feedback sameAs アイス・アルベド・フィードバック.
- Ice-albedo_feedback sameAs m.05f7ds8.
- Ice-albedo_feedback sameAs Q1310671.
- Ice-albedo_feedback sameAs Q1310671.
- Ice-albedo_feedback sameAs Ice-albedo_feedback.
- Ice-albedo_feedback wasDerivedFrom Ice-albedo_feedback?oldid=602340355.
- Ice-albedo_feedback depiction Greenland_Albedo_Change.png.
- Ice-albedo_feedback isPrimaryTopicOf Ice-albedo_feedback.