Thomas Rackow

The Arctic has warmed nearly four times faster than the globe since 1979

The Anthropocene as a Geological Time Unit

Defining the onset of the Anthropocene

Arctic Warming Revealed by Multiple CMIP6 Models: Evaluation of Historical Simulations and Quantification of Future Projection Uncertainties

Arctic Sea Ice in CMIP6

A simulation of small to giant Antarctic iceberg evolution: Differential impact on climatology estimates

Antarctic Sea Ice Area in CMIP6

Twenty first century changes in Antarctic and Southern Ocean surface climate in CMIP6