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Ocean output of TMI model Pleistocene Milankovitch cycle experiments |
TY - DATA
T1 - Ocean output of TMI model Pleistocene Milankovitch cycle experiments
AU - Morée, Anne
AU - Sun, Tianyi
AU - Bretones, Anaïs
AU - Straume, Eivind
AU - Nisancioglu, Kerim
AU - Gebbie, Geoffrey
AU - Geophysical Institute, University of Bergen
AU - Jackson School of Geosciences, the University of Texas at Austin
AU - Department of Earth Science, University of Bergen
AU - Centre for Earth Evolution and Dynamics, University of Oslo
AU - Department of Physical Oceanography, Woods Hole Oceanographic Institution
PY - 2021
PB - Norstore
UR - https://doi.org/10.11582/2021.00001
DO - 10.11582/2021.00001
ER -
Morée, A., Sun, T., Bretones, A., Straume, E., Nisancioglu, K., Gebbie, G., Geophysical Institute, University of Bergen, Jackson School of Geosciences, the University of Texas at Austin, Department of Earth Science, University of Bergen, Centre for Earth Evolution and Dynamics, University of Oslo, Department of Physical Oceanography, Woods Hole Oceanographic Institution (2021).Ocean output of TMI model Pleistocene Milankovitch cycle experiments [Data set]. Norstore. https://doi.org/10.11582/2021.00001
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| Published |
2021-01-04 |
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(20.07 GB)
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| Description |
Model results for the experiments done with the TMI (version 7) model. The North Atlantic (within 50-80°N and 100°W-20°E) and Southern Ocean (≥ 60°S) were forced at the air-sea boundary with normalized Pleistocene (2 Ma to present) solar insolation timeseries at 65°N and 65°S respectively, for 200 kyr. The model had a 200y time step and the time resolution is therefore a 1000 time steps. The relative strength of the North Atlantic and Southern Ocean sources (the S/N ratio) is explored in the different experiments (listed under attribute experiment_id_list), by multiplication of the Southern Ocean insolation forcing with the S/N ratio. See the Morée et al. Paper in Geophysical research letters ‘Cancellation of the precessional cycle in δ18O records during the Early Pleistocene’ for further details on the model, the model forcing and the model experiments.
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Science publication
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