TOPOI-CS_ECHAM5

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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(2019) . TOPOI-CS_ECHAM5. https://gdk.gdi-de.org/geonetwork/srv/api/records/wdc-climate.de:3843800

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File identifier: wdc-climate.de:3843800 XML

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code: TOPOI-CS_ECHAM5

code: doi:10.26050/WDCC/TOPOI-CS_ECHAM5

Metadata language: eng; USA

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ECHAM5

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paleoclimate simulation

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Date ( Publication ): 2019-10-02

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Organisation name: Freie Universität Berlin

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Organisation name: Freie Universität Berlin

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Organisation name: Freie Universität Berlin

Organisation name: Freie Universität Berlin

Date stamp: 2019-04-16T17:09:04

Metadata language: eng; USA

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