[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 …

Human influence on the climate system (Chapter 3)

V Eyring, NP Gillett, KM Achuta Rao, R Barimalala… - 2021 - pure.iiasa.ac.at
The AR5 concluded that human influence on the climate system is clear, evident from
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …

Framing, Context, and Methods (Chapter 1)

D Chen, M Rojas, BH Samset, K Cobb… - 2021 - pure.iiasa.ac.at
Working Group I (WGI) of the Intergovernmental Panel on Climate Change (IPCC) assesses
the current evidence on the physical science of climate change, evaluating knowledge …

[HTML][HTML] Multi-centennial Holocene climate variability in proxy records and transient model simulations

TG Askjær, Q Zhang, F Schenk, FC Ljungqvist… - Quaternary Science …, 2022 - Elsevier
Variability on centennial to multi-centennial timescales is mentioned as a feature in
reconstructions of the Holocene climate. As more long transient model simulations with …

[HTML][HTML] Large-scale features and evaluation of the PMIP4-CMIP6 midHolocene simulations

CM Brierley, A Zhao, SP Harrison, P Braconnot… - Climate of the …, 2020 - cp.copernicus.org
The mid-Holocene (6000 years ago) is a standard experiment for the evaluation of the
simulated response of global climate models using paleoclimate reconstructions. The latest …

[HTML][HTML] Large-scale features of Last Interglacial climate: results from evaluating the lig127k simulations for the Coupled Model Intercomparison Project (CMIP6) …

BL Otto-Bliesner, EC Brady, A Zhao… - Climate of the …, 2021 - cp.copernicus.org
The modeling of paleoclimate, using physically based tools, is increasingly seen as a strong
out-of-sample test of the models that are used for the projection of future climate changes …

[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 …

[HTML][HTML] Comparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models

JR Brown, CM Brierley, SI An, MV Guarino… - Climate of the …, 2020 - cp.copernicus.org
El Niño–Southern Oscillation (ENSO) is the strongest mode of interannual climate variability
in the current climate, influencing ecosystems, agriculture, and weather systems across the …

The PMIP4 contribution to CMIP6 – Part 3: The last millennium, scientific objective, and experimental design for the PMIP4 past1000 simulations

JH Jungclaus, E Bard, M Baroni… - Geoscientific Model …, 2017 - gmd.copernicus.org
The pre-industrial millennium is among the periods selected by the Paleoclimate Model
Intercomparison Project (PMIP) for experiments contributing to the sixth phase of the …

[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 …