Abstract
An abnormally cold winter across the southern half of Greenland led to substantially higher west coast sea ice thickness and concentration. Even so, record-setting summer temperatures around Greenland, combined with an intense melt season (particularly across the northern ice sheet), led the 2008 Greenland climate to be marked by continued ice sheet mass deficit and marine- terminating ice disintegration.
| Original language | English |
|---|---|
| Title of host publication | Changes in the Arctic |
| Subtitle of host publication | Background and issues |
| Editors | Brandon D. Swarson |
| Publisher | Nova Science Publishers, Inc. |
| Pages | 91-99 |
| Number of pages | 9 |
| ISBN (Electronic) | 9781617610394 |
| ISBN (Print) | 9781617288821 |
| Publication status | Published - 2010 |
| Externally published | Yes |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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SDG 14 Life Below Water
Programme Area
- Programme Area 5: Nature and Climate
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