This model study sets out to investigate how the collapse of the Greenland ice sheet to a virtually ice-free state due to increasing temperatures depends on the rate of this increase. We find oscillations in ice volume on millennial timescales that impact the time it takes before the ice sheet collapses, concluding that there is a mode of deterministic chaos internal to the ice sheet dynamics…
Source: European Geosciences Union (EGU)
European Geosciences Union (EGU)
- Livestock grazing, plant community and abiotic factors shape blue carbon stocks in Nordic coastal marshes
- In-depth characterisation of organic matter thermal lability and composition from Arctic Permafrost thaw slumps
- Review article: The Foundation-Patuxent-Academy ice stream system, Antarctica
- Understanding changes in Iceland's streamflow dynamics in response to climate change
- Detection and attribution of the role of anthropogenic climate change in industrial-era retreat of Pine Island Glacier
- Quantification of inmixing of Asian Monsoon air by multi-species classification in a match flight experiment
- Climate models with moderate climate sensitivity best simulate the magnitude of Earth's energy imbalance
- Air–Sea Interactions and Biogeochemical Responses to Medicane Daniel
- Influence of tropospheric temperature on the formation and aging of secondary organic aerosol from biogenic vapor mixtures
- Estuarine mixing
