This README.txt file was generated on Feb 9 2021 by Anna Ruth Halberstadt ------------------- GENERAL INFORMATION ------------------- 1. Title of Dataset: Model data for 'CO2 and Tectonic Controls on Antarctic Climate and Ice-Sheet Evolution in the Mid-Miocene' 2. Author Information First Author Contact Information Name: Anna Ruth W Halberstadt Institution: University of Massachusetts Amherst Address: Department of Geosciences, University of Massachusetts, Amherst, Massachusetts 01003, USA Email: ahalberstadt@umass.edu --------------------- DATA & FILE OVERVIEW --------------------- Description of Dataset: This dataset contains the source data for the following publication: 'CO2 and Tectonic Controls on Antarctic Climate and Ice-Sheet Evolution in the Mid-Miocene' by Halberstadt et al. [full citation, doi] We use an ensemble of asynchronously coupled climate - ice sheet - vegetation model simulations spanning a range of CO2 concentrations, Transantarctic Mountain uplift scenarios, and glacial/interglacial climatic conditions to identify climate and ice-sheet conditions consistent with Antarctic mid-Miocene terrestrial and marine geological records. Here we provide the final equilibrated output data for each model ensemble member. List of Directories: A. Directory: ISMs Short description: Ice Sheet Model output Header information for model output variables is contained in the text file ISM.example.vars.txt B. Directory: GCMs Short description: Global Climate Model output Header information for model output variables is contained in the text file GCM.example.vars.txt C. Directory: RCMs Short description: Regional Climate Model output Header information for model output variables is contained in the text file RCM.example.vars.txt File Naming Convention: All model output is in netcdf format, and is named according to the boundary conditions used: [1. model type][2. CO2][3. topography and orbit] 1. Model type: refers to either ice sheet model ('ISM'; Pollard and DeConto, 2012), regional climate model ('RCM', RegCM; Pal et al., 2007), or global climate model ('GCM', GENESIS version 3.0; Thompson and Pollard, 1997). More information about each model and the coupling details can be found in the Supplementary Materials corresponding to the primary publication (listed above). 2. CO2: refers to the CO2 boundary condition specified in the RCM and GCM; files are named after the CO2 values set in the model where all the radiative forcing is driven by CO2 rather than other greenhouse gases (see discussion of 'model CO2' and 'effective CO2' in the publication main text and Supplementary Materials for more information). Therefore, file names containing model CO2 ('280','500','840','1000','1200','1500') correspond to effective CO2 values discussed in the publication of '280','460','690','780','930','1140' ppm, respectively. 3. Topography and orbit: refers to the input topography where the Transantarctic Mountains are either left unchanged from the Paxman et al. (2019) reconstruction of 14 Ma median paleotopography ('norm'), hinged downwards by 300m, 500m, or 800m ('h300','h500', or 'h800'), or hinged upwards by 300m ('h300U'). All model data are run under a 'interglacial' climate favorable for Antarctic deglaciation (a warm astronomical orbit) except for the model runs named 'ncold' which denotes an unchanged topography and a 'glacial' climate favorable for Antarctic glaciation (a warm astronomical orbit). See the publication main text and Supplementary Materials for more information on topopraphic modifications and astronomical orbit. For example, an ice-sheet model output with 280ppm CO2, a warm orbit, and topography hinged downwards by 800m is named: 'ISM.280h800.nc' --------------------- REFERENCES --------------------- Pollard, D., DeConto, R.M., 2012. Description of a hybrid ice sheet-shelf model, and application to Antarctica. Geosci. Model Dev. 5, 1273–1295. https://doi.org/10.5194/gmd-5-1273-2012 Pal, J.S., Giorgi, F., Bi, X., Elguindi, N., Solmon, F., Gao, X., Rauscher, S.A., Francisco, R., Zakey, A., Winter, J., others, 2007. Regional climate modeling for the developing world: the ICTP RegCM3 and RegCNET. Bull. Am. Meteorol. Soc. 88, 1395–1410. Thompson, S.L., Pollard, D., 1997. Ice-sheet mass balance at the Last Glacial maximum from the GENESIS version 2 global climate model. Ann. Glaciol. 25. https://doi.org/10.3189/s0260305500268109 Paxman, G.J.G., Jamieson, S.S.R., Hochmuth, K., Gohl, K., Bentley, M.J., Leitchenkov, G., Ferraccioli, F., 2019. Reconstructions of Antarctic topography since the Eocene–Oligocene boundary. Palaeogeogr. Palaeoclimatol. Palaeoecol. 535, 109346. https://doi.org/10.1016/j.palaeo.2019.109346