Articles | Volume 13, issue 10
https://doi.org/10.5194/cp-13-1323-2017
© Author(s) 2017. 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-13-1323-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Oct 2017
Research article |
| 11 Oct 2017
| 11 Oct 2017
Does δ18O of O2 record meridional shifts in tropical rainfall?
Scripps Institution of Oceanography, University of
California-San Diego, La Jolla, CA 92037, USA
Christo Buizert
College of Earth, Ocean and Atmospheric Sciences, Oregon
State University, Corvallis, OR 97331, USA
Daniel Baggenstos
Climate and Environmental Physics, University of Bern, 3012 Bern, Switzerland
Edward J. Brook
College of Earth, Ocean and Atmospheric Sciences, Oregon
State University, Corvallis, OR 97331, USA
Jinho Ahn
School of Earth and Environmental Sciences, Seoul National
University, Seoul 08826, South Korea
Ji-Woong Yang
School of Earth and Environmental Sciences, Seoul National
University, Seoul 08826, South Korea
Jeffrey P. Severinghaus
Scripps Institution of Oceanography, University of
California-San Diego, La Jolla, CA 92037, USA
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- Fractionation of O<sub>2</sub>∕N<sub>2</sub> and Ar∕N<sub>2</sub> in the Antarctic ice sheet during bubble formation and bubble–clathrate hydrate transition from precise gas measurements of the Dome Fuji ice core I. Oyabu et al. 10.5194/tc-15-5529-2021
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- Chronostratigraphy of the Larsen blue-ice area in northern Victoria Land, East Antarctica, and its implications for paleoclimate G. Lee et al. 10.5194/tc-16-2301-2022
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- Dole effect as a measurement of the low-latitude hydrological cycle over the past 800 ka E. Huang et al. 10.1126/sciadv.aba4823
- On the use of δ18Oatm for ice core dating T. Extier et al. 10.1016/j.quascirev.2018.02.008
- Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
- Controls on Millennial‐Scale Atmospheric CO2 Variability During the Last Glacial Period T. Bauska et al. 10.1029/2018GL077881
- An 83 000-year-old ice core from Roosevelt Island, Ross Sea, Antarctica J. Lee et al. 10.5194/cp-16-1691-2020
- Antarctic surface temperature and elevation during the Last Glacial Maximum C. Buizert et al. 10.1126/science.abd2897
- Multi-phased Asian hydroclimate variability during Heinrich Stadial 5 D. Liu et al. 10.1007/s00382-022-06566-w
- Clumped‐Isotope Constraint on Upper‐Tropospheric Cooling During the Last Glacial Maximum A. Banerjee et al. 10.1029/2022AV000688
- Atmospheric methane variability through the Last Glacial Maximum and deglaciation mainly controlled by tropical sources B. Riddell-Young et al. 10.1038/s41561-023-01332-x
- Millennial‐Scale Changes in Terrestrial and Marine Nitrous Oxide Emissions at the Onset and Termination of Marine Isotope Stage 4 J. Menking et al. 10.1029/2020GL089110
- Water Source Signatures in the Spatial and Seasonal Isotope Variation of Chinese Tap Waters S. Wang et al. 10.1029/2018WR023091
- Stable Hydrogen and Oxygen Isotope Characteristics of Bottled Water in China: A Consideration of Water Source R. Guo et al. 10.3390/w11051065
- The strength, position, and width changes of the intertropical convergence zone since the Last Glacial Maximum S. Yuan et al. 10.1073/pnas.2217064120
25 citations as recorded by crossref.
- Is the Noble Gas‐Based Rate of Ocean Warming During the Younger Dryas Overestimated? S. Shackleton et al. 10.1029/2019GL082971
- Stable Isotope Reveals Tap Water Source under Different Water Supply Modes in the Eastern Margin of the Qinghai–Tibet Plateau M. Du et al. 10.3390/w11122578
- A Horizontal Ice Core From Taylor Glacier, Its Implications for Antarctic Climate History, and an Improved Taylor Dome Ice Core Time Scale D. Baggenstos et al. 10.1029/2017PA003297
- New technique for high-precision, simultaneous measurements of CH<sub>4</sub>, N<sub>2</sub>O and CO<sub>2</sub> concentrations; isotopic and elemental ratios of N<sub>2</sub>, O<sub>2</sub> and Ar; and total air content in ice cores by wet extraction I. Oyabu et al. 10.5194/amt-13-6703-2020
- Discrimination in Tree Stems O2 Uptake and the Dole Effect B. Hilman & A. Angert 10.1029/2018GB005918
- Southward Shift of the Pacific ITCZ During the Holocene J. Sachs et al. 10.1029/2018PA003469
- Fractionation of O<sub>2</sub>∕N<sub>2</sub> and Ar∕N<sub>2</sub> in the Antarctic ice sheet during bubble formation and bubble–clathrate hydrate transition from precise gas measurements of the Dome Fuji ice core I. Oyabu et al. 10.5194/tc-15-5529-2021
- Coupled atmosphere-ice-ocean dynamics during Heinrich Stadial 2 X. Dong et al. 10.1038/s41467-022-33583-4
- Chronostratigraphy of the Larsen blue-ice area in northern Victoria Land, East Antarctica, and its implications for paleoclimate G. Lee et al. 10.5194/tc-16-2301-2022
- Use of δ 18 O atm in dating a Tibetan ice core record of Holocene/Late Glacial climate L. Thompson et al. 10.1073/pnas.2205545119
- The isotopic composition of the French Illimani ice core in the Bolivian Andes supports the east-west South American precipitation dipole from the last deglaciation to the mid-Holocene F. Vimeux & A. Landais 10.1016/j.quascirev.2024.109098
- Unveiling the anatomy of Termination 3 using water and air isotopes in the Dome C ice core, East Antarctica C. Bréant et al. 10.1016/j.quascirev.2019.03.025
- Dole effect as a measurement of the low-latitude hydrological cycle over the past 800 ka E. Huang et al. 10.1126/sciadv.aba4823
- On the use of δ18Oatm for ice core dating T. Extier et al. 10.1016/j.quascirev.2018.02.008
- Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
- Controls on Millennial‐Scale Atmospheric CO2 Variability During the Last Glacial Period T. Bauska et al. 10.1029/2018GL077881
- An 83 000-year-old ice core from Roosevelt Island, Ross Sea, Antarctica J. Lee et al. 10.5194/cp-16-1691-2020
- Antarctic surface temperature and elevation during the Last Glacial Maximum C. Buizert et al. 10.1126/science.abd2897
- Multi-phased Asian hydroclimate variability during Heinrich Stadial 5 D. Liu et al. 10.1007/s00382-022-06566-w
- Clumped‐Isotope Constraint on Upper‐Tropospheric Cooling During the Last Glacial Maximum A. Banerjee et al. 10.1029/2022AV000688
- Atmospheric methane variability through the Last Glacial Maximum and deglaciation mainly controlled by tropical sources B. Riddell-Young et al. 10.1038/s41561-023-01332-x
- Millennial‐Scale Changes in Terrestrial and Marine Nitrous Oxide Emissions at the Onset and Termination of Marine Isotope Stage 4 J. Menking et al. 10.1029/2020GL089110
- Water Source Signatures in the Spatial and Seasonal Isotope Variation of Chinese Tap Waters S. Wang et al. 10.1029/2018WR023091
- Stable Hydrogen and Oxygen Isotope Characteristics of Bottled Water in China: A Consideration of Water Source R. Guo et al. 10.3390/w11051065
- The strength, position, and width changes of the intertropical convergence zone since the Last Glacial Maximum S. Yuan et al. 10.1073/pnas.2217064120
Latest update: 14 Dec 2024
Short summary
To explore whether the oxygen-18 to oxygen-16 ratio of atmospheric O2 is sensitive to the position of the tropical rain belts, we (1) present a record of ice core bubble oxygen isotope measurements from two Antarctic ice cores, and (2) examine the sensitivity of oxygen isotopes in precipitation, weighted by photosynthesis, to the location of oxygen production over the modern-day seasonal cycle. We find a strong modern relationship and discuss implications for past shifts in tropical rainfall.
To explore whether the oxygen-18 to oxygen-16 ratio of atmospheric O2 is sensitive to the...
