This chapter assesses simulations of future global climate change, spanning time horizons from the near term (2021–2040), mid-term (2041–2060), and long term (2081–2100) out to …
T Mauritsen, J Bader, T Becker… - Journal of Advances …, 2019 - Wiley Online Library
A new release of the Max Planck Institute for Meteorology Earth System Model version 1.2 (MPI‐ESM1. 2) is presented. The development focused on correcting errors in and …
We formalize the Gaia hypothesis about the Earth climate system using advances in theoretical biology based on the minimization of variational free energy. This amounts to the …
Some climate variables do not show the same response to declining atmospheric CO2 concentrations as before the preceding increase. A comprehensive understanding of this …
Climate models have continued to be developed and improved since the AR4, and many models have been extended into Earth System models by including the representation of …
Polar temperatures over the last several million years have, at times, been slightly warmer than today, yet global mean sea level has been 6–9 metres higher as recently as the Last …
MA Giorgetta, J Jungclaus, CH Reick… - Journal of Advances …, 2013 - Wiley Online Library
The new Max‐Planck‐Institute Earth System Model (MPI‐ESM) is used in the Coupled Model Intercomparison Project phase 5 (CMIP5) in a series of climate change experiments …
B Stevens, M Giorgetta, M Esch… - Journal of Advances …, 2013 - Wiley Online Library
ECHAM6, the sixth generation of the atmospheric general circulation model ECHAM, is described. Major changes with respect to its predecessor affect the representation of …
The early Earth's environment is controversial. Climatic estimates range from hot to glacial, and inferred marine pH spans strongly alkaline to acidic. Better understanding of early …