Simulating Arctic Climate Warmth and Icefield Retreat in the Last Interglaciation
Ice field
Greenland ice sheet
Ice-sheet model
Arctic geoengineering
DOI:
10.1126/science.1120808
Publication Date:
2006-03-23T21:53:12Z
AUTHORS (6)
ABSTRACT
In the future, Arctic warming and melting of polar glaciers will be considerable, but magnitude both is uncertain. We used a global climate model, dynamic ice sheet paleoclimatic data to evaluate Northern Hemisphere high-latitude its impact on icefields during Last Interglaciation. Our simulated matches observations past warming, combination physically based ice-sheet modeling with ice-core constraints indicate that Greenland Ice Sheet other circum-Arctic fields likely contributed 2.2 3.4 meters sea-level rise
SUPPLEMENTAL MATERIAL
Coming soon ....
REFERENCES (31)
CITATIONS (793)
EXTERNAL LINKS
PlumX Metrics
RECOMMENDATIONS
FAIR ASSESSMENT
Coming soon ....
JUPYTER LAB
Coming soon ....