Yushiro Fujii, Kenji Satake, Shin’ichi Sakai, Masanao Shinohara, and Toshihiko Kanazawa (2011), Tsunami source of the 2011 off the Pacific coast of Tohoku Earthquake, Earth Planets Space, 63, 815–820, doi:10.5047/eps.2011.06.010 This paper compiled t… もっと読む
Suito (2017) developed a three-dimensional viscoelastic model using Finite Element Method to understand the postseismic deformation that followed the 2011 Tohoku-Oki earthquake and to clarify which elements of the viscoelastic media affect the observ… もっと読む
地球磁場の国際標準モデルであるIGRF(International Geomagnetic Reference Field)モデルは、国際地球電磁気学会(IAGA)の第5分科会(Division V)・地磁気モデル作業委員会(Working Group V-MOD: Geomagnetic Field Modeling)により、5年ごとに新しいバージョンが発表されることになっています。現在の最新版である第12世代(12th generation)は2014年12月に発表され、それに関する論文の特… もっと読む
Suzuki et al. (2016) have conducted waveform inversion to infer the three-dimensional (3-D) S-velocity structure in the lowermost 400 km of the mantle (the D'' region) beneath the Northern Pacific region. The 3-D S-velocity model obtained in this stu… もっと読む
Together with geodetic and seismic inversions of subsurface fault slip for the 2016 Mw = 7.0 16 April 2016 Kumamoto earthquake, Toda et al. (2016) present a schematic structural model where oblique motion occurred on a northwest-dipping subsurface fa… もっと読む
Time-lapse monitoring of seismic velocity at volcanic areas can provide unique insight into the property of hydrothermal and magmatic fluids and their temporal variability. Taira and Brenguier (2016) established a quasi real-time velocity monitoring system by using seismic interferometry with ambient noise to explore the temporal evolution of velocity in the Lassen Volcanic Center, Northern California. もっと読む
About 40 tracking stations all over the world are currently operational for Satellite Laser Ranging (SLR), a very precise geodetic technique. Otsubo et al. (2016) ran a unique simulation to find the optimal place of a future SLR station. The answer depends on a geodetic product and one example is shown for the center of gravity of the Earth: the X and Y components are largely improved by a high-latitude station especially in the southern hemisphere, whereas the Z component is improved by a low-latitude station. もっと読む
