Articles | Volume 17, issue 3
https://doi.org/10.5194/cp-17-1119-2021
© 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-17-1119-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Jun 2021
Research article |
| 04 Jun 2021
| 04 Jun 2021
A data–model approach to interpreting speleothem oxygen isotope records from monsoon regions
Sarah E. Parker
CORRESPONDING AUTHOR
School of Archaeology, Geography and Environmental Science, University of Reading, Reading, UK
Sandy P. Harrison
School of Archaeology, Geography and Environmental Science, University of Reading, Reading, UK
Laia Comas-Bru
School of Archaeology, Geography and Environmental Science, University of Reading, Reading, UK
Nikita Kaushal
Asian School of the Environment, Nanyang Technological University, Singapore, Singapore
Allegra N. LeGrande
NASA Goddard Institute for Space Studies and Center for Climate
Systems Research, Columbia University, New York, USA
Martin Werner
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Bremerhaven, Germany
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Cited
15 citations as recorded by crossref.
- Speleothem records of monsoon interannual-interdecadal variability through the Holocene S. Parker et al. 10.1088/2515-7620/ac3eaa
- Process‐Based Intercomparison of Water Isotope‐Enabled Models and Reanalysis Nudging Effects H. Bong et al. 10.1029/2023JD038719
- Rapid Climate Links Between High Northern Latitudes and Tropical Southeast Asia Over the Last 40 ka J. Huang et al. 10.1029/2023GL107171
- Altitude effect of precipitation isotopes in an arid mountain-basin system: Observation and modelling around the world’s second-largest shifting desert S. Wang et al. 10.1016/j.jhydrol.2024.131351
- 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
- Interannual variations in stable isotopes of atmospheric water in arid Central Asia due to changes in atmospheric circulation S. Wang et al. 10.1016/j.gloplacha.2024.104367
- Precipitation Oxygen Isotope Changes Over East Asia Driven by Sea Surface Conditions During the Last Glacial Maximum H. Lan et al. 10.1029/2023PA004692
- Orbitally forced and internal changes in West African rainfall interannual-to-decadal variability for the last 6000 years J. Crétat et al. 10.1007/s00382-023-07023-y
- The SISAL webApp: exploring the speleothem climate and environmental archives of the world I. Hatvani et al. 10.1017/qua.2023.39
- Quaternary rainfall variability is governed by insolation in northern China and ice-sheet forcing in the South D. Zhao et al. 10.1038/s43247-022-00670-9
- SISALv3: a global speleothem stable isotope and trace element database N. Kaushal et al. 10.5194/essd-16-1933-2024
- Model-based orbital-scale precipitation δ18O variations and distinct mechanisms in Asian monsoon and arid regions X. Liu et al. 10.1093/nsr/nwac182
- Precession-driven changes in air-sea CO2 exchange by East Asian summer monsoon in the Western Tropical Pacific since MIS 6 J. Guo et al. 10.1016/j.palaeo.2022.111267
- The timing, duration and magnitude of the 8.2 ka event in global speleothem records S. Parker & S. Harrison 10.1038/s41598-022-14684-y
- Comparison of the oxygen isotope signatures in speleothem records and iHadCM3 model simulations for the last millennium J. Bühler et al. 10.5194/cp-17-985-2021
14 citations as recorded by crossref.
- Speleothem records of monsoon interannual-interdecadal variability through the Holocene S. Parker et al. 10.1088/2515-7620/ac3eaa
- Process‐Based Intercomparison of Water Isotope‐Enabled Models and Reanalysis Nudging Effects H. Bong et al. 10.1029/2023JD038719
- Rapid Climate Links Between High Northern Latitudes and Tropical Southeast Asia Over the Last 40 ka J. Huang et al. 10.1029/2023GL107171
- Altitude effect of precipitation isotopes in an arid mountain-basin system: Observation and modelling around the world’s second-largest shifting desert S. Wang et al. 10.1016/j.jhydrol.2024.131351
- 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
- Interannual variations in stable isotopes of atmospheric water in arid Central Asia due to changes in atmospheric circulation S. Wang et al. 10.1016/j.gloplacha.2024.104367
- Precipitation Oxygen Isotope Changes Over East Asia Driven by Sea Surface Conditions During the Last Glacial Maximum H. Lan et al. 10.1029/2023PA004692
- Orbitally forced and internal changes in West African rainfall interannual-to-decadal variability for the last 6000 years J. Crétat et al. 10.1007/s00382-023-07023-y
- The SISAL webApp: exploring the speleothem climate and environmental archives of the world I. Hatvani et al. 10.1017/qua.2023.39
- Quaternary rainfall variability is governed by insolation in northern China and ice-sheet forcing in the South D. Zhao et al. 10.1038/s43247-022-00670-9
- SISALv3: a global speleothem stable isotope and trace element database N. Kaushal et al. 10.5194/essd-16-1933-2024
- Model-based orbital-scale precipitation δ18O variations and distinct mechanisms in Asian monsoon and arid regions X. Liu et al. 10.1093/nsr/nwac182
- Precession-driven changes in air-sea CO2 exchange by East Asian summer monsoon in the Western Tropical Pacific since MIS 6 J. Guo et al. 10.1016/j.palaeo.2022.111267
- The timing, duration and magnitude of the 8.2 ka event in global speleothem records S. Parker & S. Harrison 10.1038/s41598-022-14684-y
Latest update: 23 Nov 2024
Short summary
Regional trends in the oxygen isotope (δ18O) composition of stalagmites reflect several climate processes. We compare stalagmite δ18O records from monsoon regions and model simulations to identify the causes of δ18O variability over the last 12 000 years, and between glacial and interglacial states. Precipitation changes explain the glacial–interglacial δ18O changes in all monsoon regions; Holocene trends are due to a combination of precipitation, atmospheric circulation and temperature changes.
Regional trends in the oxygen isotope (δ18O) composition of stalagmites reflect several climate...
