Model Output for "Isolated Northern Hemisphere Cooling in an Idealized Model Promotes Ocean Carbon Storage and Glacial-like Ocean Features"

Please cite the Journal of Climate article (Shankle et al. 2026) if using this output. Included is the final 1000 years of output from the control and three experiment simulations ran in Shankle et al. 2026 (JClim): Glac_Ref = run_SouthWarm.Ctrl_1000yr15_wSIdiags/ IG_Ctrl = run_SouthWarm.100percNAwarm_1000yr15_wSIdiags/ IG_N50 = run_SouthWarm.050percNAwarm_1000yr15_wSIdiags/ IG_N100 = run_SouthWarm.000percNAwarm_1000yr15_wSIdiags/ (The naming of the directories follows a previous scheme. E.g., cooling the northern latitudes all the way to glacial-like temperatures (100% or "IG_N100" in the paper) == 0% northern warming.) Also included is the output from a simulation where only high southern latitudes are cooled and text files giving the evolution of atmospheric pCO$_2$ in each simulation (value given at end of each 1000 years).Scripts to analyse this output are available on M. Shankle's GitHub (https://github.com/Maddie-Sh).