Articles | Volume 17, issue 3
https://doi.org/10.5194/cp-17-985-2021
© 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-17-985-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 May 2021
Research article |
| 05 May 2021
| 05 May 2021
Comparison of the oxygen isotope signatures in speleothem records and iHadCM3 model simulations for the last millennium
Janica C. Bühler
CORRESPONDING AUTHOR
Institute of Environmental Physics, Ruprecht-Karls-Universität Heidelberg, INF 229, 69120 Heidelberg, Germany
Carla Roesch
Institute of Environmental Physics, Ruprecht-Karls-Universität Heidelberg, INF 229, 69120 Heidelberg, Germany
Moritz Kirschner
Institute of Environmental Physics, Ruprecht-Karls-Universität Heidelberg, INF 229, 69120 Heidelberg, Germany
Louise Sime
British Arctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, United Kingdom
Max D. Holloway
Scottish Association for Marine Science, Scottish Marine Institute, Oban, Argyll, PA37 1QA, United Kingdom
Kira Rehfeld
CORRESPONDING AUTHOR
Institute of Environmental Physics, Ruprecht-Karls-Universität Heidelberg, INF 229, 69120 Heidelberg, Germany
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Cited
13 citations as recorded by crossref.
- Probing the timescale dependency of local and global variations in surface air temperature from climate simulations and reconstructions of the last millennia B. Ellerhoff & K. Rehfeld 10.1103/PhysRevE.104.064136
- The SISAL webApp: exploring the speleothem climate and environmental archives of the world I. Hatvani et al. 10.1017/qua.2023.39
- Investigating stable oxygen and carbon isotopic variability in speleothem records over the last millennium using multiple isotope-enabled climate models J. Bühler et al. 10.5194/cp-18-1625-2022
- Millennial-scale climate variability in the Northern Hemisphere influenced glacier dynamics in the Alps around 250,000 years ago V. Skiba et al. 10.1038/s43247-023-01083-y
- Identifying Global‐Scale Patterns of Vegetation Change During the Last Deglaciation From Paleoclimate Networks M. Adam et al. 10.1029/2021PA004265
- A continental reconstruction of hydroclimatic variability in South America during the past 2000 years M. Choblet et al. 10.5194/cp-20-2117-2024
- Regional but not global temperature variability underestimated by climate models at supradecadal timescales T. Laepple et al. 10.1038/s41561-023-01299-9
- Process‐Based Intercomparison of Water Isotope‐Enabled Models and Reanalysis Nudging Effects H. Bong et al. 10.1029/2023JD038719
- Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation N. Weitzel et al. 10.5194/cp-20-865-2024
- Interpreting precipitation δ18O over eastern China for the Asian summer monsoon: Results from the last millennium simulations Y. Liu et al. 10.1002/joc.8171
- Speleothems in subglacial caves: An emerging archive of glacial climate history and mountain glacier dynamics C. Spötl et al. 10.1016/j.quascirev.2024.108684
- TransEBM v. 1.0: description, tuning, and validation of a transient model of the Earth's energy balance in two dimensions E. Ziegler & K. Rehfeld 10.5194/gmd-14-2843-2021
- Contrasting State‐Dependent Effects of Natural Forcing on Global and Local Climate Variability B. Ellerhoff et al. 10.1029/2022GL098335
11 citations as recorded by crossref.
- Probing the timescale dependency of local and global variations in surface air temperature from climate simulations and reconstructions of the last millennia B. Ellerhoff & K. Rehfeld 10.1103/PhysRevE.104.064136
- The SISAL webApp: exploring the speleothem climate and environmental archives of the world I. Hatvani et al. 10.1017/qua.2023.39
- Investigating stable oxygen and carbon isotopic variability in speleothem records over the last millennium using multiple isotope-enabled climate models J. Bühler et al. 10.5194/cp-18-1625-2022
- Millennial-scale climate variability in the Northern Hemisphere influenced glacier dynamics in the Alps around 250,000 years ago V. Skiba et al. 10.1038/s43247-023-01083-y
- Identifying Global‐Scale Patterns of Vegetation Change During the Last Deglaciation From Paleoclimate Networks M. Adam et al. 10.1029/2021PA004265
- A continental reconstruction of hydroclimatic variability in South America during the past 2000 years M. Choblet et al. 10.5194/cp-20-2117-2024
- Regional but not global temperature variability underestimated by climate models at supradecadal timescales T. Laepple et al. 10.1038/s41561-023-01299-9
- Process‐Based Intercomparison of Water Isotope‐Enabled Models and Reanalysis Nudging Effects H. Bong et al. 10.1029/2023JD038719
- Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation N. Weitzel et al. 10.5194/cp-20-865-2024
- Interpreting precipitation δ18O over eastern China for the Asian summer monsoon: Results from the last millennium simulations Y. Liu et al. 10.1002/joc.8171
- Speleothems in subglacial caves: An emerging archive of glacial climate history and mountain glacier dynamics C. Spötl et al. 10.1016/j.quascirev.2024.108684
2 citations as recorded by crossref.
- TransEBM v. 1.0: description, tuning, and validation of a transient model of the Earth's energy balance in two dimensions E. Ziegler & K. Rehfeld 10.5194/gmd-14-2843-2021
- Contrasting State‐Dependent Effects of Natural Forcing on Global and Local Climate Variability B. Ellerhoff et al. 10.1029/2022GL098335
Latest update: 23 Nov 2024
Short summary
We present three new isotope-enabled simulations for the last millennium (850–1850 CE) and compare them to records from a global speleothem database. Offsets between the simulated and measured oxygen isotope ratios are fairly small. While modeled oxygen isotope ratios are more variable on decadal timescales, proxy records are more variable on (multi-)centennial timescales. This could be due to a lack of long-term variability in complex model simulations, but proxy biases cannot be excluded.
We present three new isotope-enabled simulations for the last millennium (850–1850 CE) and...
