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.
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
Data sets
Accumulation rate, volcanic tie points, ECM, DEP, nssSO4, density and chronology from shallow ice cores around Dome Fuji, East Antarctica I. Oyabu, K. Kawamura, S. Fujita, R. Inoue, H. Motoyama, N. Kurita, F.Nakazawa, H. Ohno, K. Sugiura, T. Suzuki, S. Tsutaki, A. Abe-Ouchi, M. Niwano, F. Parrenin, F. Saito, and M. Yoshimori https://doi.org/10.17592/001.2022081901
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...