Articles | Volume 13, issue 2
https://doi.org/10.5194/cp-13-107-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-107-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Biome changes in Asia since the mid-Holocene – an analysis of different transient Earth system model simulations
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
Meteorological Institute, Centrum für Erdsystemforschung und
Nachhaltigkeit (CEN), Universität Hamburg, Bundesstraße 55, 20146
Hamburg, Germany
Institute of Biochemistry and Biology, University of Potsdam,
Maulbeerallee 3, 14469 Potsdam, Germany
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Telegrafenberg A43, 14473 Potsdam, Germany
State Key Laboratory of Environmental Geochemistry, Institute of
Geochemistry, Chinese Academy of Sciences, Lincheng West Road 99, 550081
Guiyang, China
Xianyong Cao
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Telegrafenberg A43, 14473 Potsdam, Germany
Institute of Earth and Environmental Science, University of Potsdam,
Karl-Liebknecht-Straße 24–25, 14476 Potsdam, Germany
Yongbo Wang
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Telegrafenberg A43, 14473 Potsdam, Germany
College of Resource Environment and Tourism, Capital Normal
University, Beijing 100048, China
Nils Fischer
Max Planck Institute for Meteorology, Bundesstraße 53, 20146 Hamburg,
Germany
Madlene Pfeiffer
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, 27568 Bremerhaven, Germany
Liya Jin
Key Laboratory of Western China's Environmental Systems, College of
Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
Vyacheslav Khon
Institute of Geosciences, Christian-Albrechts Universität zu
Kiel, Ludewig-Meyn-Str. 10–14, 24118 Kiel, Germany
A. M. Obukhov Institute of Atmospheric Physics RAS, Pyzhevsky 3,
117019 Moscow, Russia
Sebastian Wagner
Helmholtz Center Geesthacht, Institute for Coastal Research, 21502
Geesthacht, Germany
Kerstin Haberkorn
Meteorological Institute, Centrum für Erdsystemforschung und
Nachhaltigkeit (CEN), Universität Hamburg, Bundesstraße 55, 20146
Hamburg, Germany
Ulrike Herzschuh
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Telegrafenberg A43, 14473 Potsdam, Germany
Institute of Earth and Environmental Science, University of Potsdam,
Karl-Liebknecht-Straße 24–25, 14476 Potsdam, Germany
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Cited
20 citations as recorded by crossref.
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- Environmental change since the Last Glacial Maximum: palaeo‐evidence from the Nee Soon Freshwater Swamp Forest, Singapore C. Nguyen et al. 10.1002/jqs.3403
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- Pollen spectrum, a cornerstone for tracing the evolution of the eastern Central Asian desert K. Lu et al. 10.1016/j.quascirev.2018.02.009
- Mid-Holocene climate change over China: model–data discrepancy Y. Lin et al. 10.5194/cp-15-1223-2019
- Harmonising plant functional type distributions for evaluating Earth system models A. Dallmeyer et al. 10.5194/cp-15-335-2019
- A Possible Role of Dust in Resolving the Holocene Temperature Conundrum Y. Liu et al. 10.1038/s41598-018-22841-5
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- Eurasian Holocene climate trends in transient coupled climate simulations and stable oxygen isotope records C. DANEK et al. 10.1002/jqs.3396
- Comparison of climate responses to orbital forcing at different latitudes during the Holocene Y. Jing et al. 10.1016/j.quaint.2022.02.004
- Identifying long-term stable refugia for dominant Castanopsis species of evergreen broad-leaved forests in East Asia: A tool for ensuring their conservation C. Tang et al. 10.1016/j.biocon.2022.109663
- Progress of vegetation modelling and future research prospects S. Li et al. 10.1007/s11430-023-1367-1
- Long-term decrease in Asian monsoon rainfall and abrupt climate change events over the past 6,700 years B. Yang et al. 10.1073/pnas.2102007118
- Demographic History and Genomic Response to Environmental Changes in a Rapid Radiation of Wild Rats D. Ge et al. 10.1093/molbev/msaa334
- IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations P. Sepulchre et al. 10.5194/gmd-13-3011-2020
- 植被模型研究进展与展望 思. 李 et al. 10.1360/SSTe-2023-0204
- How to map biomes: Quantitative comparison and review of biome‐mapping methods A. Champreux et al. 10.1002/ecm.1615
- Northern Hemisphere biome changes (>30°N) since 40 cal ka BP and their driving factors inferred from model-data comparisons X. Cao et al. 10.1016/j.quascirev.2019.07.034
- Holocene changes in biomass burning in the boreal Northern Hemisphere, reconstructed from anhydrosugar fluxes in an Arctic sediment profile A. Chen et al. 10.1016/j.scitotenv.2023.161460
20 citations as recorded by crossref.
- Biome changes and their inferred climatic drivers in northern and eastern continental Asia at selected times since 40 cal ka bp F. Tian et al. 10.1007/s00334-017-0653-8
- Environmental change since the Last Glacial Maximum: palaeo‐evidence from the Nee Soon Freshwater Swamp Forest, Singapore C. Nguyen et al. 10.1002/jqs.3403
- Refining data–data and data–model vegetation comparisons using the Earth mover's distance (EMD) M. Chevalier et al. 10.5194/cp-19-1043-2023
- Pollen spectrum, a cornerstone for tracing the evolution of the eastern Central Asian desert K. Lu et al. 10.1016/j.quascirev.2018.02.009
- Mid-Holocene climate change over China: model–data discrepancy Y. Lin et al. 10.5194/cp-15-1223-2019
- Harmonising plant functional type distributions for evaluating Earth system models A. Dallmeyer et al. 10.5194/cp-15-335-2019
- A Possible Role of Dust in Resolving the Holocene Temperature Conundrum Y. Liu et al. 10.1038/s41598-018-22841-5
- Russian Climate Research in 2015–2018 I. Mokhov 10.1134/S0001433820040064
- Neoglacial climate anomalies and the Harappan metamorphosis L. Giosan et al. 10.5194/cp-14-1669-2018
- Eurasian Holocene climate trends in transient coupled climate simulations and stable oxygen isotope records C. DANEK et al. 10.1002/jqs.3396
- Comparison of climate responses to orbital forcing at different latitudes during the Holocene Y. Jing et al. 10.1016/j.quaint.2022.02.004
- Identifying long-term stable refugia for dominant Castanopsis species of evergreen broad-leaved forests in East Asia: A tool for ensuring their conservation C. Tang et al. 10.1016/j.biocon.2022.109663
- Progress of vegetation modelling and future research prospects S. Li et al. 10.1007/s11430-023-1367-1
- Long-term decrease in Asian monsoon rainfall and abrupt climate change events over the past 6,700 years B. Yang et al. 10.1073/pnas.2102007118
- Demographic History and Genomic Response to Environmental Changes in a Rapid Radiation of Wild Rats D. Ge et al. 10.1093/molbev/msaa334
- IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations P. Sepulchre et al. 10.5194/gmd-13-3011-2020
- 植被模型研究进展与展望 思. 李 et al. 10.1360/SSTe-2023-0204
- How to map biomes: Quantitative comparison and review of biome‐mapping methods A. Champreux et al. 10.1002/ecm.1615
- Northern Hemisphere biome changes (>30°N) since 40 cal ka BP and their driving factors inferred from model-data comparisons X. Cao et al. 10.1016/j.quascirev.2019.07.034
- Holocene changes in biomass burning in the boreal Northern Hemisphere, reconstructed from anhydrosugar fluxes in an Arctic sediment profile A. Chen et al. 10.1016/j.scitotenv.2023.161460
Latest update: 15 Nov 2024
Short summary
The vegetation distribution in eastern Asia is supposed to be very sensitive to climate change. Since proxy records are scarce, hitherto a mechanistic understanding of the past spatio-temporal climate–vegetation relationship is lacking. To assess the Holocene vegetation change, we forced the diagnostic biome model BIOME4 with climate anomalies of different transient climate simulations.
The vegetation distribution in eastern Asia is supposed to be very sensitive to climate change....