Arctic climate: changes in sea ice extent outweigh changes in snow cover
<p>Recent declines in Arctic sea ice and snow extent have led to an increase in the absorption of solar energy at the surface, resulting in additional surface heating and a further decline in snow and ice. Using 34 years of satellite data, 1982–2015, we found that the positive trend in sola...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-10-01
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| Series: | The Cryosphere |
| Online Access: | https://www.the-cryosphere.net/12/3373/2018/tc-12-3373-2018.pdf |
| Summary: | <p>Recent declines in Arctic sea ice and snow extent have led to an increase in
the absorption of solar energy at the surface, resulting in additional
surface heating and a further decline in snow and ice. Using 34 years of
satellite data, 1982–2015, we found that the positive trend in solar
absorption over the Arctic Ocean is more than double that over Arctic land,
and the magnitude of the ice–albedo feedback is four times that of the
snow–albedo feedback in summer. The timing of the high-to-low albedo
transition has shifted closer to the greater insolation of the summer
solstice over ocean, but further away from the summer solstice over land.
Therefore, decreasing sea ice cover, not changes in terrestrial snow cover,
has been the dominant radiative feedback mechanism over the last few decades.</p> |
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| ISSN: | 1994-0416 1994-0424 |