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Merkel, Ute; Prange, Matthias; Schulz, Michael (2012): Glacial ENSO and Atlantic Meridional Overturning Circulation - Link to model results. PANGAEA, https://doi.org/10.1594/PANGAEA.786514, Supplement to: Merkel, U et al. (2010): ENSO variability and teleconnections during glacial climates. Quaternary Science Reviews, 29(1-2), 86-100, https://doi.org/10.1016/j.quascirev.2009.11.006

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Abstract:
Numerical experiments using the general circulation model CCSM3 have been performed for glacial climates: Last Glacial Maximum (LGM), Heinrich Stadial 1 (HS1), Marine Isotope Stage 3 Stadial (MIS3-ST) and Marine Isotope Stage 3 Interstadial (MIS3-IST). As a reference, a control simulation for preindustrial climate (PI) has been performed. Details of the experiments are described in Merkel et al. (2010).
The datasets contain timeseries from the last 100 years of each model simulation.
For each experiment, we present:
- annual mean timeseries of the maximum of the Atlantic Meridional Overturning Circulation between 30°N and 80°N and below 500 m.
- monthly mean timeseries of sea surface temperature area-averaged over the Nino3-region (5°S-5°N, 150°W-90°W).
Coverage:
Median Latitude: 20.625000 * Median Longitude: -120.000000 * South-bound Latitude: -5.000000 * West-bound Longitude: -150.000000 * North-bound Latitude: 80.000000 * East-bound Longitude: -90.000000
Comment:
Coverage for this collection of datasets is determined automatically through averaging by Pangaea. Since this collection contains data from very different geographic areas, users should check the actual coverage from the information given on the websites of the individual datasets.
Project: Research project SCHU1389/6-1 of the Deutsche Forschungsgemeinschaft (DFG) and DFG-Research Center/Excellence Cluster "The Ocean in the Earth System - MARUM".
Size:
2 datasets

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