Abstract
The Greenland ice sheet's response to climate change is a major issue in the climate debate. This report reviews existing evidence on how the ice sheet margins reacted to climate change during the past 300,000 years-how it responded to the warm climate of the last interglacial and expanded on to the shelf during the last ice age. Compared to the other large ice sheets in the northern hemisphere, the Greenland ice sheet showed remarkable resilience to temperature change-a good omen for the future.
| Original language | English |
|---|---|
| Title of host publication | Quaternary Glaciations - Extent and Chronology |
| Subtitle of host publication | A Closer Look |
| Editors | Jürgen Ehlers, Philip L. Gibbard, Philip D. Hughes |
| Publisher | Elsevier |
| Chapter | 50 |
| Pages | 699-713 |
| Number of pages | 15 |
| ISBN (Electronic) | 978-0-444-53447-7 |
| DOIs | |
| Publication status | Published - 2011 |
| Externally published | Yes |
Publication series
| Series | Developments in Quaternary Science |
|---|---|
| Volume | 15 |
| ISSN | 1571-0866 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
-
SDG 13 Climate Action
Keywords
- Climate change
- Greenland ice sheet
- Ice sheet stability
- Interglacial/glacial
- Mid-Late Pleistocene
Programme Area
- Programme Area 5: Nature and Climate
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