Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q1310671> ?p ?o }
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- Q1310671 subject Q7143452.
- Q1310671 subject Q8383143.
- Q1310671 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.".
- Q1310671 thumbnail Greenland_Albedo_Change.png?width=300.
- Q1310671 wikiPageWikiLink Q101038.
- Q1310671 wikiPageWikiLink Q1161410.
- Q1310671 wikiPageWikiLink Q125465.
- Q1310671 wikiPageWikiLink Q16243069.
- Q1310671 wikiPageWikiLink Q213926.
- Q1310671 wikiPageWikiLink Q23392.
- Q1310671 wikiPageWikiLink Q35666.
- Q1310671 wikiPageWikiLink Q521783.
- Q1310671 wikiPageWikiLink Q7143452.
- Q1310671 wikiPageWikiLink Q7209060.
- Q1310671 wikiPageWikiLink Q7209100.
- Q1310671 wikiPageWikiLink Q8383143.
- Q1310671 wikiPageWikiLink Q841083.
- Q1310671 wikiPageWikiLink Q878077.
- Q1310671 wikiPageWikiLink Q918004.
- Q1310671 wikiPageWikiLink Q952151.
- Q1310671 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.".
- Q1310671 label "Ice-albedo feedback".
- Q1310671 depiction Greenland_Albedo_Change.png.