File:Permafrost thaw ESA19399520.jpeg
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|DescriptionPermafrost thaw ESA19399520.jpeg||
English: Ponds resulting from thawing permafrost in the Yamal Peninsula in northwest Siberia captured by the Copernicus Sentinel-2 mission on 27 August 2018. In Earth’s cold regions, much of the sub-surface ground is frozen. Permafrost is frozen soil, rock or sediment – sometimes hundreds of metres thick. To be classified as permafrost, the ground has to have been frozen for at least two years, but much of the sub-surface ground in the polar regions has been frozen since the last ice age.
Permafrost holds carbon-based remains of vegetation and animals that froze before they could decompose. Scientists estimate that the world’s permafrost holds almost double the amount of carbon that is currently in the atmosphere. When permafrost warms and thaws, it releases methane and carbon dioxide, adding these greenhouse gases to the atmosphere and making global warming even worse.
|Date||17 May 2019 (upload date)|
|Author||European Space Agency|
|Activity||Observing the Earth|
|Set||Living Planet Symposium 2019|
|This image contains data from a satellite in the Copernicus Programme, such as Sentinel-1, Sentinel-2 or Sentinel-3. Attribution is required when using this image.
Attribution: Contains modified Copernicus Sentinel data 2018 Attribution
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|Number of components||3|
|Horizontal resolution||1 dpi|
|Vertical resolution||1 dpi|
|Data arrangement||chunky format|
|Software used||Adobe Photoshop CC 2019 (Windows)|
|File change date and time||11:30, 9 May 2019|
|Date and time of digitizing||13:16, 9 May 2019|
|Date metadata was last modified||13:30, 9 May 2019|
|Unique ID of original document||xmp.did:3644b4fd-058b-8547-a925-c6c818ea45b4|