Articles | Volume 16, issue 11
Atmos. Chem. Phys., 16, 6883–6900, 2016
https://doi.org/10.5194/acp-16-6883-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 6883–6900, 2016
https://doi.org/10.5194/acp-16-6883-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article 06 Jun 2016
Research article | 06 Jun 2016
Precipitation regime and stable isotopes at Dome Fuji, East Antarctica
Anna Dittmann et al.
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Cited
16 citations as recorded by crossref.
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- Acquisition of Post-Depositional Effects on Stable Isotopes (δ18O and δD) of Snow and Firn at Dome A, East Antarctica T. Ma et al. 10.3390/w12061707
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- The influence of the synoptic regime on stable water isotopes in precipitation at Dome C, East Antarctica E. Schlosser et al. 10.5194/tc-11-2345-2017
- Surface mass balance and water stable isotopes derived from firn cores on three ice rises, Fimbul Ice Shelf, Antarctica C. Vega et al. 10.5194/tc-10-2763-2016
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14 citations as recorded by crossref.
- Water stable isotope spatio-temporal variability in Antarctica in 1960–2013: observations and simulations from the ECHAM5-wiso atmospheric general circulation model S. Goursaud et al. 10.5194/cp-14-923-2018
- Evaluation of Seasonal and Synoptic Changes in Snow Accumulation in Antarctica between Five Reanalyses Products and In Situ Observations Y. Liu et al. 10.3390/atmos9120473
- Mass balance of the ice sheets and glaciers – Progress since AR5 and challenges E. Hanna et al. 10.1016/j.earscirev.2019.102976
- Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica S. Goursaud et al. 10.5194/tc-13-1297-2019
- Atmospheric moisture pathways of East Africa and implications for water recycling at Mount Kilimanjaro B. Schumacher et al. 10.1002/joc.6468
- Seasonal Deuterium Excess Variations of Precipitation at Summit, Greenland, and their Climatological Significance B. Kopec et al. 10.1029/2018JD028750
- Environmental significance and zonal characteristics of stable isotope of atmospheric precipitation in arid Central Asia Z. Li et al. 10.1016/j.atmosres.2019.04.022
- Precipitation regime influence on oxygen triple-isotope distributions in Antarctic precipitation and ice cores M. Miller 10.1016/j.epsl.2017.10.035
- Antarctic climate variability on regional and continental scales over the last 2000 years B. Stenni et al. 10.5194/cp-13-1609-2017
- Acquisition of Post-Depositional Effects on Stable Isotopes (δ18O and δD) of Snow and Firn at Dome A, East Antarctica T. Ma et al. 10.3390/w12061707
- Climatic information archived in ice cores: impact of intermittency and diffusion on the recorded isotopic signal in Antarctica M. Casado et al. 10.5194/cp-16-1581-2020
- The influence of the synoptic regime on stable water isotopes in precipitation at Dome C, East Antarctica E. Schlosser et al. 10.5194/tc-11-2345-2017
- Surface mass balance and water stable isotopes derived from firn cores on three ice rises, Fimbul Ice Shelf, Antarctica C. Vega et al. 10.5194/tc-10-2763-2016
- Intra-Event Isotopic Changes in Water Vapor and Precipitation in South China X. Li et al. 10.3390/w13070940
2 citations as recorded by crossref.
- Precipitation and synoptic regime in two extreme years 2009 and 2010 at Dome C, Antarctica – implications for ice core interpretation E. Schlosser et al. 10.5194/acp-16-4757-2016
- Tropical precipitation anomalies and d -excess evolution during El Niño 2014-16 R. Sánchez-Murillo et al. 10.1002/hyp.11088
Saved (preprint)
Latest update: 03 Aug 2021
Short summary
For a better understanding of the stable water isotope data from ice cores, recent time periods have to be analysed, where both measurements and model simulations are available. This was done for Dome Fuji by combining observations, synoptic analysis, back trajectories, and isotopic modelling. It was found that a more northerly moisture source does not necessarily mean a larger temperature difference between source area and deposition site and thus precipitation more depleted in heavy isotopes.
For a better understanding of the stable water isotope data from ice cores, recent time periods...
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