Japan Geoscience Union Meeting 2016

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-CG Complex & General

[S-CG59] Ocean Floor Geoscience

Wed. May 25, 2016 1:45 PM - 3:15 PM 301B (3F)

Convener:*Kyoko Okino(Ocean Research Institute, University of Tokyo), Keiichi Tadokoro(Research Center for Seismology, Volcanology and Earthquake and Volcano Research Center, Nagoya University), Osamu Ishizuka(Geological Survey of Japan, AIST), Tomohiro Toki(Faculty of Science, University of the Ryukyus), Narumi Takahashi(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology), Chair:Yojiro Yamamoto(Japan Agency for Marine-Earth Science and Technology), Mikiya Yamashita(Japan Agency for Marine-Earth Science and Technology)

2:00 PM - 2:15 PM

[SCG59-02] Accuracy of GPS-Acoustic seafloor geodetic observation evaluated by numerical simulation

*Toshiharu Tashiro1, Tadashi Ishikawa1, Yusuke Yokota1, Shun-ichi Watanabe1 (1.Japan Coast Guard)

Keywords:seafloor geodetic observation, GPS-Acoustic combination technique

Hydrographic and Oceanographic Department, Japan Coast Guard (JHOD), has been carrying out seafloor geodetic observations with the GPS-Acoustic combination technique (GPS-A), in order to detect a displacesment of a focal area of the interplate earthquake. For example, we detected coseismic displacements, long-term interseismic and postsesmic deformations [e.g., Sato et al., 2011].
However, insufficient frequency of the observation (a few times per year) prevents us from detecting the short-term deformation due to slow slip events and time-dependent postseismic effects. Therefore, it is necessary to improve the accuracy and/or frequency of the observation under the condition of limited ship-time. For the purpose of improving the frequency, we tested the alternative survey lines to optimize the accuracy and geometrical simplicity simultaneously, using pseudo GPS-A data generated by the GPS-A simulator [Yokota et al., 2016]. This simulator can generate the pseudo observation data sets with any errors and obtain the pseudo positions of seafloor transponder by inversion analysis.
In this presentation, we report the results of the accuracy of the alternative survey line, comparing the results using actual observation data.