Articles | Volume 17, issue 6
Clim. Past, 17, 2481–2513, 2021
https://doi.org/10.5194/cp-17-2481-2021
Clim. Past, 17, 2481–2513, 2021
https://doi.org/10.5194/cp-17-2481-2021
Research article
02 Dec 2021
Research article | 02 Dec 2021

Holocene vegetation transitions and their climatic drivers in MPI-ESM1.2

Anne Dallmeyer et al.

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Cited articles

Bader, J., Jungclaus, J., Krivova, N., Lorenz, S., Maycock, A., Raddatz, T., Schmidt, H., Toohey, M., Wu, C.-J, and Claussen, M.: Global temperature modes shed light on the Holocene temperature conundrum, Nat. Commun., 11, 4726, https://doi.org/10.1038/s41467-020-18478-6, 2020. 
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Bartlein, P. J. and Shafer, S. L.: Paleo calendar-effect adjustments in time-slice and transient climate-model simulations (PaleoCalAdjust v1.0): impact and strategies for data analysis, Geosci. Model Dev., 12, 3889–3913, https://doi.org/10.5194/gmd-12-3889-2019, 2019. 
Behling, H. and Hooghiemstra, H.: Neotropical savanna environments in space and time: Late Quaternary interhemispheric comparisons, chap. 18, in: Interhemispheric Climate Linkages, edited by: Markgraf, V., Academic Press, San Diego, USA, 2001. 
Berger, A. L.: Long-term variations of daily insolation and quater-nary climatic changes, J. Atmos. Sci., 35, 2362–2367, 1978. 
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Short summary
Using the comprehensive Earth system model, MPI-ESM1.2, we explore the global Holocene vegetation changes and interpret them in terms of the Holocene climate change. The model results reveal that most of the Holocene vegetation transitions seen outside the high northern latitudes can be attributed to modifications in the intensity of the global summer monsoons.