PaleoWeather: An Accelerated Scientific Discovery Project (ASD)

An unprecedented set of fully coupled high-resolution (HR) paleoclimate simulations has been performed using the water isotope-enabled Community Earth System Model version 1.3 (iCESM1.3). The simulations include well-studied paleoclimate intervals with higher atmospheric CO2 of the Early Eocene Climatic Optimum (EECO, ~50 Ma) and mid-Pliocene Warm Period (mPWP, ~3 Ma), and lower CO2 of the Last Glacial Maximum (LGM, 21 ka), as well as a corresponding Preindustrial (PI, 1850 CE). The simulations complement historical (1850-2005), abrupt 4xCO2, and RCP8.5 future (2006-2100) simulations available from the iHESP/MESACLIP project to connect past and future climate changes.

The research goals are to study the characteristics and dynamics of extremes weather events in Earth's past and future climates, as well as the climatic impact from directly resolving fine-scale processes such as ocean eddies and tropical cyclones. The project was made possible by computing resources from an award from the NSF NCAR Accelerated Scientific Discovery (ASD). 

Project leads: Bette Otto-Bliesner (NSF NCAR) and Jessica Tierney (U of Arizona)

Project investigators and contributors:

  • Jiang Zhu: Model development and testing; preindustrial and Eocene simulations; post-processing
  • Ran Feng: Pliocene simulation; post-processing
  • Clay Tabor: LGM simulation; post-processing
  • Jesse Nusbaumer: Model development
  • Jim Edwards: Model porting and engineering support
  • Esther Brady: Simulation setup
  • Sophia Macarewich: Data Manager

Ongoing research and lead PIs:

  • Bette Otto-Bliesner & Esther Brady: Tropical cyclones in paleoclimates (* main reference for the set of simulations)
  • Jiang Zhu: Sea-surface temperatures in extreme warm climates due to resolving ocean eddies
  • Jiang Zhu & Hui Li: Role of tropical cyclones on the sea-surface temperature in equable climates
  • Ran Feng & Mary Grace Albright: Mesoscale convective systems in paleoclimates
  • Sophia Macarewich: Atmospheric rivers in paleoclimates
  • Ingrid Romero & Scott Wing: Preindustrial climate as a predictor of historical forest distributions in the US

Model: iCESM1.3_hires

Resolution: ~0.25° (~25 km) for the atmosphere and land models, and ~0.1° (~10 km at the Equator down to ~4 km at high latitudes) for the ocean and sea-ice models.

Simulations:

Name Length (years) Simulation Protocols Contributor
PI 28* CMIP Zhu
LGM 100 PMIP4 Tabor
Pliocene 60 PlioMIP2 Feng
Eocene 60 DeepMIP Zhu

* Branched off from a 22-year long PI on a different machine, which was branched off from the iHESP/MESACLIP PI of 646 years.

Policy and Data Acquisition: At this stage (before the publish of the main paper, Otto-Bliesner et al.), we are releasing the monthly output for collaborative use. Users are encouraged to provide co-authorship of papers and presentations to those who performed the simulations (Zhu for PI and Eocene, Tabor for LGM, and Feng for Pliocene) and leads of the ASD proposal and model development (Otto-Bliesner, Tierney, and Zhu). Please submit your request here.