Nine PlioMIP2 experiments were conducted to investigate the mid-Pliocene Arctic climate. These experiments considered three CO2 levels (280, 400 and 560 ppm), modern or Pliocene ice sheet conditions in Greenland and Antarctica and either prescribed or dynamic vegetation. Simulations were performed by the EC-Earth3-LR Veg climate model with a horizontal resolution of ~1.125°. The dataset contains selected output data from the simulations. Simulations were run for 1000 years. The last 200 years were used for analysis after the model reached an equilibrium as measured by global surface air temperature trend less than 0.05 K per century. The dataset contains Earth system model results from EC-Earth3 presented in the study by Power et al. (202...
We present results from modelling of the mid-Pliocene warm period (3.3–3 million years ago) using th...
The mid-Pliocene Warm Period (3.29 to 2.97 Ma BP) has been identified as an analogue for the future,...
Climate model simulations available from the PMIP1, PMIP2 and CMIP (IPCC-AR4) intercomparison projec...
Palaeoclimate simulations improve our understanding of the climate, inform us about the performance ...
International audienceThe Pliocene Model Intercomparison Project (PlioMIP) is the first coordinated ...
Here, for the first time, we present simulations of mid-Pliocene climate using a UK IPCC AR5-class m...
Accumulations of global proxy data are essential steps for improving reliability of climate model si...
As global warming is proceeding due to rising greenhouse gas concentrations, the Earth system moves ...
Ice sheets are important components of the Earth system that are expected to respond strongly to ant...
Abstract Three new equilibrium mid‐Pliocene (MP) simulations are implemented with the Community Clim...
International audienceThe Pliocene epoch has great potential to improve our understanding of the lon...
International audienceThis paper describes the experimental design and model results of the climate ...
Climate model simulations available from the PMIP1, PMIP2 and CMIP (IPCC-AR4) intercomparison projec...
The Mid-Pliocene (ca 3 Myr ago) was a relatively warm period, with increased atmospheric CO2 relativ...
The Arctic is one of the regions that experienced the fastest and highest warming of the planet duri...
We present results from modelling of the mid-Pliocene warm period (3.3–3 million years ago) using th...
The mid-Pliocene Warm Period (3.29 to 2.97 Ma BP) has been identified as an analogue for the future,...
Climate model simulations available from the PMIP1, PMIP2 and CMIP (IPCC-AR4) intercomparison projec...
Palaeoclimate simulations improve our understanding of the climate, inform us about the performance ...
International audienceThe Pliocene Model Intercomparison Project (PlioMIP) is the first coordinated ...
Here, for the first time, we present simulations of mid-Pliocene climate using a UK IPCC AR5-class m...
Accumulations of global proxy data are essential steps for improving reliability of climate model si...
As global warming is proceeding due to rising greenhouse gas concentrations, the Earth system moves ...
Ice sheets are important components of the Earth system that are expected to respond strongly to ant...
Abstract Three new equilibrium mid‐Pliocene (MP) simulations are implemented with the Community Clim...
International audienceThe Pliocene epoch has great potential to improve our understanding of the lon...
International audienceThis paper describes the experimental design and model results of the climate ...
Climate model simulations available from the PMIP1, PMIP2 and CMIP (IPCC-AR4) intercomparison projec...
The Mid-Pliocene (ca 3 Myr ago) was a relatively warm period, with increased atmospheric CO2 relativ...
The Arctic is one of the regions that experienced the fastest and highest warming of the planet duri...
We present results from modelling of the mid-Pliocene warm period (3.3–3 million years ago) using th...
The mid-Pliocene Warm Period (3.29 to 2.97 Ma BP) has been identified as an analogue for the future,...
Climate model simulations available from the PMIP1, PMIP2 and CMIP (IPCC-AR4) intercomparison projec...