TOPOI-CS_ECHAM5

Abstract:
Global paleoclimate simulations are carried out on the basis of the so-called time slice technique. The simulations are performed with the state-of-the-art global circulation model ECHAM5 (Roeckner et al., 2003) at a spectral resolution of T106 (∼1.125°×1.125°) and 19 vertical levels. Different time slices are selected at a time interval of approx. 1000 years from each other, from 6000 years ago to pre-industrial times. For each time slice a simulation is carried out over a period of 30 years. As boundary conditions prescribed sea ice fraction and sea surface temperatures were used, which were derived from a continuous simulation with transient periods. This simulation was performed with the coupled atmosphere-ocean circulation model ECHO-G, consisting of the ECHAM4 (Roeckner et al., 1996) and the ocean model HOPE (Wolff et al., 1997), at a spectral resolution of T30 (∼3.75◦×3.75◦). Further information on simulation realization can be found in Wagner et al. (2007). Detailed information on the model set-up can be found in Russo and Cubasch (2016). Russo, E. and Cubasch, U.: Mid-to-late Holocene temperature evolution and atmospheric dynamics over Europe in regional model simulations, Clim. Past, 12, 1645-1662, https://doi.org/10.5194/cp-12-1645-2016, 2016.

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Metadata Information

General

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  • TOPOI-CS_ECHAM5
contactsee section contact (role: pointOfContact)
dateStamp 2020-10-04T01:33:12
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citation
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    • TOPOI-CS_ECHAM5
  • dates:
    • creation: 2019-04-16
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    • doi:10.26050/WDCC/TOPOI-CS_ECHAM5
abstract see above
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    • paleoclimate simulation
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    • ECHAM5
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Contact

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individualNameM.Sc. Markus Thürkow
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