2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
The AR5 concluded that human influence on the climate system is clear, evident from increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
DJ Lunt, F Bragg, WL Chan, DK Hutchinson… - Climate of the …, 2021 - cp.copernicus.org
We present results from an ensemble of eight climate models, each of which has carried out simulations of the early Eocene climate optimum (EECO,∼ 50 million years ago). These …
Accurate estimates of past global mean surface temperature (GMST) help to contextualise future climate change and are required to estimate the sensitivity of the climate system to …
P Sepulchre, A Caubel, JB Ladant… - Geoscientific Model …, 2019 - gmd.copernicus.org
Based on the CMIP5-generation previous IPSL earth system model, we designed a new version, IPSL-CM5A2, aiming at running multi-millennial simulations typical of deep-time …
Benthic oxygen isotope records are commonly used as a proxy for global mean surface temperatures during the late Cretaceous and Cenozoic, and the resulting estimates have …
The Cenozoic inception and development of the Asian monsoons remain unclear and have generated much debate, as several hypotheses regarding circulation patterns at work in …
M Gurnis, T Yang, J Cannon, M Turner… - Computers & …, 2018 - Elsevier
Traditional plate reconstruction methodologies do not allow for plate deformation to be considered. Here we present software to construct and visualize global tectonic …