Articles | Volume 15, issue 4
https://doi.org/10.5194/cp-15-1223-2019
© Author(s) 2019. 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-15-1223-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
02 Jul 2019
Research article | Highlight paper |
| 02 Jul 2019
| 02 Jul 2019
Mid-Holocene climate change over China: model–data discrepancy
Yating Lin
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology
and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette 91191, France
University of Chinese Academy of Sciences, Beijing 100049, China
Gilles Ramstein
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette 91191, France
Haibin Wu
CORRESPONDING AUTHOR
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology
and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
CAS Center for Excellence in Life and Paleoenvironment, Beijing 100044,
China
University of Chinese Academy of Sciences, Beijing 100049, China
Raj Rani
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette 91191, France
Pascale Braconnot
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette 91191, France
Masa Kageyama
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette 91191, France
Qin Li
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology
and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
CAS Center for Excellence in Life and Paleoenvironment, Beijing 100044,
China
Yunli Luo
Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China
Ran Zhang
Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing
100029, China
Zhengtang Guo
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology
and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
CAS Center for Excellence in Life and Paleoenvironment, Beijing 100044,
China
University of Chinese Academy of Sciences, Beijing 100049, China
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Cited
17 citations as recorded by crossref.
- Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation feedbacks J. Chen et al. 10.1016/j.quascirev.2021.107136
- What Controls the Skill of General Circulation Models to Simulate the Seasonal Cycle in Water Isotopic Composition in the Tibetan Plateau Region? X. Shi et al. 10.1029/2022JD037048
- Distinctive changes of Asian–African summer monsoon in interglacial epochs and global warming scenario Y. Wang et al. 10.1007/s00382-023-07013-0
- Holocene seasonal temperature evolution and spatial variability over the Northern Hemisphere landmass W. Zhang et al. 10.1038/s41467-022-33107-0
- The contrasting effects of thermodynamic and dynamic processes on East Asian summer monsoon precipitation during the Last Glacial Maximum: a data-model comparison Y. Sun et al. 10.1007/s00382-020-05533-7
- Model-data divergence in global seasonal temperature response to astronomical insolation during the Holocene W. Zhang et al. 10.1016/j.scib.2021.09.004
- Enhanced Mid‐Holocene Vegetation Growth and Its Biophysical Feedbacks in China W. Chen et al. 10.1029/2023GL104702
- How Can Climate Models Be Used in Paleoelevation Reconstructions? S. Botsyun & T. Ehlers 10.3389/feart.2021.624542
- Global terrestrial monsoon area variations since Last Glacial Maximum based on TraCE21ka and PMIP4-CMIP6 simulations J. Wang et al. 10.1016/j.gloplacha.2023.104308
- Global Synthesis of Regional Holocene Hydroclimate Variability Using Proxy and Model Data C. Hancock et al. 10.1029/2022PA004597
- The mid-Holocene East Asian summer monsoon simulated by PMIP4-CMIP6 and PMIP3-CMIP5: Model uncertainty and its possible sources Y. Wu et al. 10.1016/j.gloplacha.2022.103986
- AMOC and Climate Responses to Dust Reduction and Greening of the Sahara during the Mid-Holocene M. Zhang et al. 10.1175/JCLI-D-20-0628.1
- Closure of tropical seaways favors the climate and vegetation in tropical Africa and South America approaching their present conditions N. Tan et al. 10.1016/j.gloplacha.2023.104351
- A Comparison of the CMIP6midHoloceneandlig127kSimulations in CESM2 B. Otto‐Bliesner et al. 10.1029/2020PA003957
- Mid-Holocene high-resolution temperature and precipitation gridded reconstructions over China: Implications for elevation-dependent temperature changes W. Chen et al. 10.1016/j.epsl.2022.117656
- Temperature Variation on the Central Tibetan Plateau Revealed by Glycerol Dialkyl Glycerol Tetraethers From the Sediment Record of Lake Linggo Co Since the Last Deglaciation Y. He et al. 10.3389/feart.2020.574206
- Revisiting the physical mechanisms of East Asian summer monsoon precipitation changes during the mid-Holocene: a data–model comparison Y. Sun et al. 10.1007/s00382-022-06359-1
17 citations as recorded by crossref.
- Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation feedbacks J. Chen et al. 10.1016/j.quascirev.2021.107136
- What Controls the Skill of General Circulation Models to Simulate the Seasonal Cycle in Water Isotopic Composition in the Tibetan Plateau Region? X. Shi et al. 10.1029/2022JD037048
- Distinctive changes of Asian–African summer monsoon in interglacial epochs and global warming scenario Y. Wang et al. 10.1007/s00382-023-07013-0
- Holocene seasonal temperature evolution and spatial variability over the Northern Hemisphere landmass W. Zhang et al. 10.1038/s41467-022-33107-0
- The contrasting effects of thermodynamic and dynamic processes on East Asian summer monsoon precipitation during the Last Glacial Maximum: a data-model comparison Y. Sun et al. 10.1007/s00382-020-05533-7
- Model-data divergence in global seasonal temperature response to astronomical insolation during the Holocene W. Zhang et al. 10.1016/j.scib.2021.09.004
- Enhanced Mid‐Holocene Vegetation Growth and Its Biophysical Feedbacks in China W. Chen et al. 10.1029/2023GL104702
- How Can Climate Models Be Used in Paleoelevation Reconstructions? S. Botsyun & T. Ehlers 10.3389/feart.2021.624542
- Global terrestrial monsoon area variations since Last Glacial Maximum based on TraCE21ka and PMIP4-CMIP6 simulations J. Wang et al. 10.1016/j.gloplacha.2023.104308
- Global Synthesis of Regional Holocene Hydroclimate Variability Using Proxy and Model Data C. Hancock et al. 10.1029/2022PA004597
- The mid-Holocene East Asian summer monsoon simulated by PMIP4-CMIP6 and PMIP3-CMIP5: Model uncertainty and its possible sources Y. Wu et al. 10.1016/j.gloplacha.2022.103986
- AMOC and Climate Responses to Dust Reduction and Greening of the Sahara during the Mid-Holocene M. Zhang et al. 10.1175/JCLI-D-20-0628.1
- Closure of tropical seaways favors the climate and vegetation in tropical Africa and South America approaching their present conditions N. Tan et al. 10.1016/j.gloplacha.2023.104351
- A Comparison of the CMIP6midHoloceneandlig127kSimulations in CESM2 B. Otto‐Bliesner et al. 10.1029/2020PA003957
- Mid-Holocene high-resolution temperature and precipitation gridded reconstructions over China: Implications for elevation-dependent temperature changes W. Chen et al. 10.1016/j.epsl.2022.117656
- Temperature Variation on the Central Tibetan Plateau Revealed by Glycerol Dialkyl Glycerol Tetraethers From the Sediment Record of Lake Linggo Co Since the Last Deglaciation Y. He et al. 10.3389/feart.2020.574206
- Revisiting the physical mechanisms of East Asian summer monsoon precipitation changes during the mid-Holocene: a data–model comparison Y. Sun et al. 10.1007/s00382-022-06359-1
Latest update: 18 Apr 2024
Short summary
The mid-Holocene has been an excellent target for comparing models and data. This work shows that, over China, all the ocean–atmosphere general circulation models involved in PMIP3 show a very large discrepancy with pollen data reconstruction when comparing annual and seasonal temperature. It demonstrates that to reconcile models and data and to capture the signature of seasonal thermal response, it is necessary to integrate non-linear processes, particularly those related to vegetation changes.
The mid-Holocene has been an excellent target for comparing models and data. This work shows...
