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)
- Estuarine mixing
- Global and diurnal variations in tropospheric ammonia observed from a constellation of hyperspectral infrared sounders in three different LEO orbits
- Chaotic fluctuations in Greenland ice streams limit predictability of ice sheet collapse
- Rapid soil degradation following deforestation in Eastern Africa
- On describing particle nucleation within the Volatility Basis Set
- Denitrification as the dominant process in nitrous oxide production in the water column of two eutrophic reservoirs
- Atmospheric river trajectories organise along a global transport network
- The Pluvial Flood Index (PFI): a new instrument for evaluating flash flood hazards and facilitating real-time warning
- Quantitative climate reconstruction from sedimentary ancient DNA: framework, validation and application
- The influence of ocean waves on Antarctic sea-ice albedo and seasonal melting, and potential coupled physical and biological feedbacks
