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)
- Historical climate extremes in Europe and the connection between spring precipitation and summer heat
- Invited perspective: Uncertainties in natural systems may be uncomfortable, but ignoring them would be absurd
- From manual classification to transformer-based language models: assessing the quality and consistency of historical convective event records
- Pokémon Trading Cards reveal visual stereotypes of natural minerals
- Decoded Antarctic snow accumulation history reconciles observed and modeled trends in accumulation and large-scale warming patterns
- Origin of low ozone above western North America: an investigation of sources and trends
- Assessing Earth system responses in mitigation scenarios with activity-driven simulation of carbon dioxide removal
- Ocean dynamics amplify remote warming effects of reforestation
- Invited Perspectives: Science for Comprehensive Disaster and Climate Risk Management
- The North American CORDEX-CMIP6 WRF evaluation run: comparing historical simulations from 25 km to convection-permitting scales
