results:transientholocenesimulations

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results:transientholocenesimulations [2021/01/11 15:15]
jungclaus [Experiment 2]
results:transientholocenesimulations [2021/01/11 15:17] (current)
jungclaus [References]
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 data accessible via http server at DKRZ on request, contact: Johann Jungclaus. Data from Brovkin et al. (2019) available from the MPI-M library by contacting publications@mpimet.mpg.de data accessible via http server at DKRZ on request, contact: Johann Jungclaus. Data from Brovkin et al. (2019) available from the MPI-M library by contacting publications@mpimet.mpg.de
 == Experiment 3 == == Experiment 3 ==
- +SLO0050 (TRAF) 
-Experiment description Transient Holocene simulation (8 ka BP to 1850 CE) with interactive vegetation, and forcing by volcanic aerosols and solar irradiance changes. +Experiment descriptionTransient Holocene simulation (8 ka BP to 1850 CE) with interactive vegetation, and forcing by volcanic aerosols and solar irradiance changes. 
 +Acces to data: data accessible via http server at DKRZ on request, contact: Johann Jungclaus.
 == Acces to data ???? == == Acces to data ???? ==
  
 == References == == References ==
 +
 +Bader, J.; Jungclaus, J.; Krivova, N.; Lorenz, S.; and Claussen, M., 2020: Global temperature modes shed light on the Holocene temperature conundrum”, Nature Communications, 11: 4726. doi:10.1038/s41467-020-18478-6 .
 +
 +Brovkin, V., Lorenz, S., Raddatz, T., Ilyina, T., Stemmler, I., Toohey, M., and Claussen, M.: What was the source of the atmospheric CO2 increase during the Holocene?, Biogeosciences, 16, 2543–2555, https://doi.org/10.5194/bg-16-2543-2019, 2019. 
  
 Dallmeyer, A. Claussen, M. , Lorenz, S.J., Shanahan, T.: The end of the African humid period as seen by a transient comprehensive Earth system model simulation of the last 8000 years, Clim. Past, 16, 117–140, doi: 10.5194/cp-16-117-2020, 2020. Dallmeyer, A. Claussen, M. , Lorenz, S.J., Shanahan, T.: The end of the African humid period as seen by a transient comprehensive Earth system model simulation of the last 8000 years, Clim. Past, 16, 117–140, doi: 10.5194/cp-16-117-2020, 2020.
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