Articles | Volume 19, issue 2
https://doi.org/10.5194/cp-19-293-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-19-293-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
02 Feb 2023
Research article |
| 02 Feb 2023
| 02 Feb 2023
Temporal variations of surface mass balance over the last 5000 years around Dome Fuji, Dronning Maud Land, East Antarctica
National Institute of Polar Research, Tokyo 190-8518, Japan
Kenji Kawamura
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced
Studies, SOKENDAI, Tokyo 190-8518, Japan
Japan Agency for Marine Science and Technology, Yokosuka 237-0061,
Japan
Shuji Fujita
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced
Studies, SOKENDAI, Tokyo 190-8518, Japan
Ryo Inoue
Department of Polar Science, The Graduate University for Advanced
Studies, SOKENDAI, Tokyo 190-8518, Japan
Hideaki Motoyama
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced
Studies, SOKENDAI, Tokyo 190-8518, Japan
Kotaro Fukui
Tateyama Caldera Sabo Museum, Toyama 930-1405, Japan
Motohiro Hirabayashi
National Institute of Polar Research, Tokyo 190-8518, Japan
Yu Hoshina
Graduate School of Environmental Studies, Nagoya University, Nagoya
464-8601, Japan
Naoyuki Kurita
Institute of Space-Earth Environmental Science, Nagoya University, Nagoya, 464-8601, Japan
Fumio Nakazawa
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced
Studies, SOKENDAI, Tokyo 190-8518, Japan
Hiroshi Ohno
School of Earth, Energy and Environmental Engineering, Kitami
Institute of Technology, Kitami 090-8507, Japan
Konosuke Sugiura
School of Sustainable Design, University of Toyama, Toyama 930-8555, Japan
Toshitaka Suzuki
Faculty of Science, Yamagata University, Yamagata 990-8560, Japan
Shun Tsutaki
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced
Studies, SOKENDAI, Tokyo 190-8518, Japan
Ayako Abe-Ouchi
Atmosphere and Ocean Research Institute, The University of Tokyo,
Kashiwa 277-8564, Japan
Masashi Niwano
Physical Meteorology Research Department, Meteorological Research
Institute, Japan Meteorological Agency, Tsukuba 305-0052, Japan
Frédéric Parrenin
Université Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, 38000
Grenoble, France
Fuyuki Saito
Japan Agency for Marine Science and Technology, Yokohama 236-0001,
Japan
Masakazu Yoshimori
Atmosphere and Ocean Research Institute, The University of Tokyo,
Kashiwa 277-8564, Japan
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Cited
8 citations as recorded by crossref.
- Spatial distribution of vertical density and microstructure profiles in near-surface firn around Dome Fuji, Antarctica R. Inoue et al. 10.5194/tc-18-425-2024
- Development and fluctuation of crystal orientation fabric in the deep sections of the Dome Fuji ice core, Antarctica: impacts of dust particles and migration recrystallization T. Saruya et al. 10.5194/tc-19-2365-2025
- The Paleochrono-1.1 probabilistic model to derive a common age model for several paleoclimatic sites using absolute and relative dating constraints F. Parrenin et al. 10.5194/gmd-17-8735-2024
- Age–depth distribution in western Dronning Maud Land, East Antarctica, and Antarctic-wide comparisons of internal reflection horizons S. Franke et al. 10.5194/tc-19-1153-2025
- Recent increase in the surface mass balance in central East Antarctica is unprecedented for the last 2000 years A. Ekaykin et al. 10.1038/s43247-024-01355-1
- A one-dimensional temperature and age modeling study for selecting the drill site of the oldest ice core near Dome Fuji, Antarctica T. Obase et al. 10.5194/tc-17-2543-2023
- The Climatological Features of Atmospheric Rivers and their Role in Water Vapor Transport in the South Polar Region K. TAKAHASHI & T. SAKAZAKI 10.2151/jmsj.2025-020
- Latitudinal difference in sulfate formation from methanesulfonate oxidation in Antarctic snow imprinted on 17O-excess signature S. Hattori et al. 10.1016/j.apgeochem.2024.105901
8 citations as recorded by crossref.
- Spatial distribution of vertical density and microstructure profiles in near-surface firn around Dome Fuji, Antarctica R. Inoue et al. 10.5194/tc-18-425-2024
- Development and fluctuation of crystal orientation fabric in the deep sections of the Dome Fuji ice core, Antarctica: impacts of dust particles and migration recrystallization T. Saruya et al. 10.5194/tc-19-2365-2025
- The Paleochrono-1.1 probabilistic model to derive a common age model for several paleoclimatic sites using absolute and relative dating constraints F. Parrenin et al. 10.5194/gmd-17-8735-2024
- Age–depth distribution in western Dronning Maud Land, East Antarctica, and Antarctic-wide comparisons of internal reflection horizons S. Franke et al. 10.5194/tc-19-1153-2025
- Recent increase in the surface mass balance in central East Antarctica is unprecedented for the last 2000 years A. Ekaykin et al. 10.1038/s43247-024-01355-1
- A one-dimensional temperature and age modeling study for selecting the drill site of the oldest ice core near Dome Fuji, Antarctica T. Obase et al. 10.5194/tc-17-2543-2023
- The Climatological Features of Atmospheric Rivers and their Role in Water Vapor Transport in the South Polar Region K. TAKAHASHI & T. SAKAZAKI 10.2151/jmsj.2025-020
- Latitudinal difference in sulfate formation from methanesulfonate oxidation in Antarctic snow imprinted on 17O-excess signature S. Hattori et al. 10.1016/j.apgeochem.2024.105901
Latest update: 30 Oct 2025
Short summary
We reconstructed accumulation rate around Dome Fuji, Antarctica, over the last 5000 years from 15 shallow ice cores and seven snow pits. We found a long-term decreasing trend in the preindustrial period, which may be associated with secular surface cooling and sea ice expansion. Centennial-scale variations were also found, which may partly be related to combinations of volcanic, solar and greenhouse gas forcings. The most rapid and intense increases of accumulation rate occurred since 1850 CE.
We reconstructed accumulation rate around Dome Fuji, Antarctica, over the last 5000 years from...
