[HTML][HTML] The PMIP4 contribution to CMIP6–Part 1: Overview and over-arching analysis plan
M Kageyama, P Braconnot, SP Harrison… - Geoscientific Model …, 2018 - gmd.copernicus.org
This paper is the first of a series of four GMD papers on the PMIP4-CMIP6 experiments. Part
2 (Otto-Bliesner et al., 2017) gives details about the two PMIP4-CMIP6 interglacial …
2 (Otto-Bliesner et al., 2017) gives details about the two PMIP4-CMIP6 interglacial …
The PMIP4-CMIP6 Last Glacial Maximum experiments: preliminary results and comparison with the PMIP3-CMIP5 simulations
M Kageyama, SP Harrison, ML Kapsch… - Climate of the Past …, 2020 - cp.copernicus.org
The Last Glacial Maximum (LGM,~ 21,000 years ago) has been a major focus for evaluating
how well state-of-the-art climate models simulate climate changes as large as those …
how well state-of-the-art climate models simulate climate changes as large as those …
A 156 kyr smoothed history of the atmospheric greenhouse gases CO2, CH4, and N2O and their radiative forcing
P Köhler, C Nehrbass-Ahles, J Schmitt… - Earth System …, 2017 - essd.copernicus.org
Continuous records of the atmospheric greenhouse gases (GHGs) CO 2, CH 4, and N 2 O
are necessary input data for transient climate simulations, and their associated radiative …
are necessary input data for transient climate simulations, and their associated radiative …
[HTML][HTML] The PMIP4 contribution to CMIP6–Part 4: Scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 …
M Kageyama, S Albani, P Braconnot… - Geoscientific Model …, 2017 - gmd.copernicus.org
The Last Glacial Maximum (LGM, 21 000 years ago) is one of the suite of paleoclimate
simulations included in the current phase of the Coupled Model Intercomparison Project …
simulations included in the current phase of the Coupled Model Intercomparison Project …
The PMIP4 contribution to CMIP6–Part 2: Two interglacials, scientific objective and experimental design for Holocene and Last Interglacial simulations
BL Otto-Bliesner, P Braconnot… - Geoscientific Model …, 2017 - gmd.copernicus.org
Two interglacial epochs are included in the suite of Paleoclimate Modeling Intercomparison
Project (PMIP4) simulations in the Coupled Model Intercomparison Project (CMIP6). The …
Project (PMIP4) simulations in the Coupled Model Intercomparison Project (CMIP6). The …
[HTML][HTML] Late glacial climate evolution in the Patagonian Andes (44–47° S) from alpine glacier modelling
Numerical glacier models applied to moraine chronologies provide an opportunity to
quantify past climate change. Here we apply a two-dimensional coupled mass balance–ice …
quantify past climate change. Here we apply a two-dimensional coupled mass balance–ice …
[HTML][HTML] Paleo calendar-effect adjustments in time-slice and transient climate-model simulations (PaleoCalAdjust v1. 0): Impact and strategies for data analysis
PJ Bartlein, SL Shafer - Geoscientific Model Development, 2019 - gmd.copernicus.org
The “paleo calendar effect” is a common expression for the impact that changes in the length
of months or seasons over time, related to changes in the eccentricity of Earth's orbit and …
of months or seasons over time, related to changes in the eccentricity of Earth's orbit and …
Reconstructing Holocene temperatures in time and space using paleoclimate data assimilation
Paleoclimatic records provide valuable information about Holocene climate, revealing
aspects of climate variability for a multitude of sites around the world. However, such data …
aspects of climate variability for a multitude of sites around the world. However, such data …
[HTML][HTML] Atmospheric methane since the last glacial maximum was driven by wetland sources
Atmospheric methane (CH 4) has changed considerably in the time between the last glacial
maximum (LGM) and the preindustrial (PI) periods. We investigate these changes in …
maximum (LGM) and the preindustrial (PI) periods. We investigate these changes in …
Connecting Antarctic sea ice to deep‐ocean circulation in modern and glacial climate simulations
A Marzocchi, MF Jansen - Geophysical Research Letters, 2017 - Wiley Online Library
Antarctic sea‐ice formation plays a key role in shaping the abyssal overturning circulation
and stratification in all ocean basins, by driving surface buoyancy loss through the …
and stratification in all ocean basins, by driving surface buoyancy loss through the …