JpGU-AGU Joint Meeting 2020

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CC Cryospheric Sciences & Cold District Environment

[A-CC38] Ice cores and paleoenvironmental modeling

convener:Ayako Abe-Ouchi(Atmosphere and Ocean Research Institute, The University of Tokyo), Ryu Uemura(Nagoya University), Kenji Kawamura(National Institute of Polar Research, Research Organization of Information and Systems), Nozomu Takeuchi(Chiba University)

[ACC38-07] A basal topographic map in the Dome Fuji area, East Antarctica, constructed from a ground-based radar survey

★Invited Papers

*Shun Tsutaki1, Shuji Fujita1,2, Kenji Kawamura1,2,3, Prasad Gogineni4, Ayako Abe-Ouchi5,1, David Braaten6, Jean-Charles Gallet7, Elisabeth Isaksson7, Brice van Liefferinge7, Kenichi Matsuoka7, Charles O’Neil4, John Paden6, Fernando Rodriguez-Morales6, Ryan Taylor4, Jie-Bang Yan4, Kumiko Goto-Azuma1,2, Ralf Greve8, Stephen Hudson7, Jack Kohler7, Shriniwas Kolpuke4, Linfeng Li4, Geir Moholdt7, Hideaki Motoyama1,2, Takashi Obase5, Fuyuki SAITO3, Kotaro FUKUI9 (1.National Institute of Polar Research, 2.The Graduate University for Advanced Studies, 3.Japan Agency for Marine-Earth Science and Technology, 4.The University of Alabama, 5.The University of Tokyo, 6.The University of Kansas, 7.Norwegian Polar Institute, 8.Hokkaido University, 9.Tateyama Caldera Sabo Museum)

Keywords:Antarctica, Bed topography, ice sheet

Knowledge gained from ice core studies is crucial to understand the past and present climate and to predict the impacts of future climate changes. The International Partnership for Ice Core Sciences (IPICS) identified that drilling deep ice cores extending back in time to 1.5 million years (Ma) is crucial to better understand the change of the periodicity of the glacial cycles from 40 thousand years (ka) to the current 100 ka during the mid-Pleistocene transition (0.9−1.2 Ma). However, continuous ice core records extending beyond 1 Ma have not been retrieved from the Antarctic ice sheet. The Dome Fuji area in East Antarctica is one of the candidate areas where we may be able to find very old ice near the bottom of the ice sheet. The Japanese Antarctic Research Expedition (JARE) has conducted deep ice corings at Dome Fuji twice in the past decades. They recovered ice cores covering ages up to about 720 ka BP. Sufficient knowledge of the basal topography is crucial to find suitable candidates based on numerical ice sheet experiments. The JARE have accumulated radar sounding data in this area since 1984 (JARE 26). In order to reveal the more detailed basal topography to find candidate site of very old ice in the Dome Fuji area, a ground-based radar survey was conducted over an area of 20,000 km2 with a line spacing of 5 km during JARE 59 (2017−2018 Antarctic summer). Based on results of these surveys, we conducted a more detailed radar survey at Dome Fuji in the 2018−2019 season as a collaboration between The University of Alabama, The University of Kansas, National Institute of Polar Research under Research Organization of Information and Systems (Japan), Norwegian Polar Institute and The University of Tokyo. we used two different radar systems for the data collection. A wideband VHF radar ice sounder developed by CReSIS, University of Kansas, and a conventional pulse-modulated VHF radar with high gain antennas from JARE. An ultrawideband microwave radar developed by the University of Alabama was used to survey shallow part of internal layers to investigate surface mass balance in the area. We investigated a distance of 2,700 km in an area of about 1,000 km2. The final spacing between the survey lines varied between 0.5 km and 0.25 km. We analyze the JARE and CReSIS radar data to construct an improved map of the basal topography in the Dome Fuji area to foster the identification of a suitable drilling site in the region.