Articles | Volume 17, issue 6
https://doi.org/10.5194/cp-17-2481-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-2481-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
02 Dec 2021
Research article |
| 02 Dec 2021
| 02 Dec 2021
Holocene vegetation transitions and their climatic drivers in MPI-ESM1.2
Anne Dallmeyer
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Bundesstrasse 53, 20146 Hamburg, Germany
Martin Claussen
Max Planck Institute for Meteorology, Bundesstrasse 53, 20146 Hamburg, Germany
Centrum für Erdsystemforschung und Nachhaltigkeit (CEN),
Universität Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany
Stephan J. Lorenz
Max Planck Institute for Meteorology, Bundesstrasse 53, 20146 Hamburg, Germany
Michael Sigl
Climate and Environmental Physics and Oeschger Centre for Climate
Change Research, University of Bern, Bern, Switzerland
Matthew Toohey
Department of Physics and Engineering Physics, University of
Saskatchewan, Saskatoon, Canada
Ulrike Herzschuh
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Potsdam, Germany
Institute of Environmental Sciences and Geography, University of
Potsdam, Potsdam, Germany
Institute of Biochemistry and Biology, University of Potsdam, Potsdam, Germany
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- Revisiting the Holocene global temperature conundrum D. Kaufman & E. Broadman 10.1038/s41586-022-05536-w
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- Were climatic forcings the main driver for mid-holocene changes in settlement dynamics on the Varamin Plain (Central Iranian Plateau)? F. Kirsten et al. 10.1371/journal.pone.0290181
- Regional pollen-based Holocene temperature and precipitation patterns depart from the Northern Hemisphere mean trends U. Herzschuh et al. 10.5194/cp-19-1481-2023
- Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11 500 years) from a bipolar ice-core array M. Sigl et al. 10.5194/essd-14-3167-2022
- On the Remote Impacts of Mid‐Holocene Saharan Vegetation on South American Hydroclimate: A Modeling Intercomparison S. Tiwari et al. 10.1029/2022GL101974
- Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene N. Specht et al. 10.5194/cp-20-1595-2024
- The challenge of comparing pollen-based quantitative vegetation reconstructions with outputs from vegetation models – a European perspective A. Dallmeyer et al. 10.5194/cp-19-1531-2023
- Thermohaline patterns of intrinsic Atlantic Multidecadal Variability in MPI-ESM-LR D. Zanchettin et al. 10.1007/s00382-023-06679-w
- A planetary boundary for green water L. Wang-Erlandsson et al. 10.1038/s43017-022-00287-8
- Diverse response of global terrestrial vegetation to astronomical forcing and CO2 during the MIS-11 and MIS-13 interglacials Q. Su et al. 10.1007/s00382-022-06308-y
- Exploring spatio-temporal patterns of palynological changes in Asia during the Holocene K. Bhatta et al. 10.3389/fevo.2023.1115784
Latest update: 16 Nov 2024
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.
Using the comprehensive Earth system model, MPI-ESM1.2, we explore the global Holocene...
