| Title |
Ocean and atmosphere output of the Bergen Climate Model experiment PTC |
TY - DATA
T1 - Ocean and atmosphere output of the Bergen Climate Model experiment PTC
AU - Furevik, Tore
AU - Bentsen, Mats
AU - Drange, Helge
AU - Thorstensen Kindern, Ina Karin
AU - Kvamstø, Nils Gunnar
AU - Sorteberg, Asgeir
AU - Flatøy, Frode
AU - Bethke, Ingo
AU - Otterå, Odd Helge
AU - Geophysical Institute, University of Bergen
AU - NORCE Norwegian Research Centre
AU - Nansen Environmental and Remote Sensing Centre
AU - Bjerknes Centre for Climate Research
PY - 2020
PB - Norstore
UR - https://doi.org/10.11582/2020.00049
DO - 10.11582/2020.00049
ER -
Furevik, T., Bentsen, M., Drange, H., Thorstensen Kindern, I. K., Kvamstø, N. G., Sorteberg, A., Flatøy, F., Bethke, I., Otterå, O. H., Geophysical Institute, University of Bergen, NORCE Norwegian Research Centre, Nansen Environmental and Remote Sensing Centre, Bjerknes Centre for Climate Research (2020).Ocean and atmosphere output of the Bergen Climate Model experiment PTC [Data set]. Norstore. https://doi.org/10.11582/2020.00049
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2020-09-22 |
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(1.16 TB)
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| Description |
Committed climate change experiment prepared for the IPCC Fourth Assessment Report. BCM2.0, (2005): atmosphere: ARPEGE V3 T63L31 (cy 22b+); ocean: NERSC-MICOM V1.0 (based on MICOM V2.8), 35 vertical layers, 1.5(E-W) X 0.5(N-S) deg. res. near equator with gradual transformation to square grid cells away from equator; sea ice: NERSC Sea Ice Model (Viscous-plastic + thermodynamic), 4 gridcells per ocean grid cell; land: ISBA ARPEGE V3 version. Experiment was initiated from model year 85 (nominal year 1850) of the control simulation (with bcm_experiment_name: PC3). The time varying forcing agents were varied based upon observations and reconstructions for the late 19th and 20th centuries. Varying forcing agents: CO2,CH4,N2O, CFC11(including other CFCs and HFCs),CFC12 and sulfate aerosols (Boucher data, only direct effect). Non-varying forcing agents: Background aerosols: black carbon, sea salt, desert dust, stratospheric and tropospheric ozone, solar irradiance (1368 W/m2) and the distribution of land cover types. No volcanic aerosols. No heat or fresh water adjustments.
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