[PDF] Top 20 Co seismic surface deformation of the 2011 off the Pacific coast of Tohoku Earthquake: Spatio temporal EOF analysis of GPS data
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Co seismic surface deformation of the 2011 off the Pacific coast of Tohoku Earthquake: Spatio temporal EOF analysis of GPS data
... gin time of the M 9.0 mainshock. The sinusoidal terms are to account for ocean tidal loading effects and any day-night weather-related effect at each station (the solid tides had already been corrected out beforehand), ... See full document
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Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9 0) estimated based on GPS data—Was the asperity in Miyagi oki ruptured?
... inversion analysis, because the modeling er- rors due to the uncertainty and heterogeneity of the physical properties of the crust, such as rigidity and Poisson’s ratio, the error of the geometry of the ... See full document
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Interplate fault slip along the Japan Trench before the occurrence of the 2011 off the Pacific coast of Tohoku Earthquake as inferred from GPS data
... this earthquake. In the case of the 2005 Miyagi earthquake, postseismic transient deformation decayed rapidly with time and ended in the middle of 2007, as is seen at the sites 950172, 950175, ... See full document
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The 2011 off the Pacific coast of Tohoku Earthquake and its aftershocks observed by GEONET
... analyzed GPS data by kinematic positioning to overcome this ...disadvantage. GPS data with 30-s sampling were processed to estimate 300-s coordinates using GIPSY ...coseismic off- set ... See full document
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Source process of the 2011 off the Pacific coast of Tohoku Earthquake with the combination of teleseismic and strong motion data
... regional analysis because of a spatially finer ...by GPS analysis (GIJ, 2011) except near the trench, where a small coseismic slip was estimated by ...of GPS data near the ... See full document
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Seismic and aseismic fault slip before and during the 2011 off the Pacific coast of Tohoku Earthquake
... the GPS data is very similar to that described by Ohtani et ...short data set, neither secular displacements nor seasonal variations are ...transient deformation field is expanded in ... See full document
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Acoustic resonance and plasma depletion detected by GPS total electron content observation after the 2011 off the Pacific coast of Tohoku Earthquake
... intense earthquake occurred at 05:46:23 UT on March 11, 2011 (US Geological Survey, ...TEC data were derived from the GPS data of GEONET—a GPS receiver array network operated by ... See full document
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Spatial distribution and focal mechanisms of aftershocks of the 2011 off the Pacific coast of Tohoku Earthquake
... foreshocks off Miyagi, were basically interplate earthquakes with thrust- type focal ...from GPS data but instead occurred in the surrounding ...large co-seismic slip associated with ... See full document
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Crustal deformation map for the 2011 off the Pacific coast of Tohoku Earthquake, detected by InSAR analysis combined with GEONET data
... GEONET data to suppress the long- wavelength noise, in which the difference between LOSs of the quick interferogram and those based on GEONET data is approximated by a bilinear function and the orig- inal ... See full document
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Coseismic and early postseismic slips associated with the 2011 off the Pacific coast of Tohoku Earthquake sequence: EOF analysis of GPS kinematic time series
... 30-s GPS data obtained from GEONET sta- tions using GIPSY software in the Precise Point Position- ing (PPP) mode (Zumberge et ...of 2011 us- ing the IGS08 reprocessed GPS orbit/clock products ... See full document
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Coupling coefficient, hierarchical structure, and earthquake cycle for the source area of the 2011 off the Pacific coast of Tohoku earthquake inferred from small repeating earthquake data
... low seismic coupling (10–30%) based on the cu- mulative seismic moment over the past ∼100 years ...However, GPS data analyses in the recent 5–7 years ...observed seismic moment release ... See full document
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Focal mechanism and slip history of the 2011 Mw 9 1 off the Pacific coast of Tohoku Earthquake, constrained with teleseismic body and surface waves
... vertical co-seismic displacement fields but also their peak ...inland GPS dataset tend to map the slip more close to the hypocenter and have a significant reduce in slip toward the trench ...al., ... See full document
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Centroid moment tensor analysis of the 2011 off the Pacific coast of Tohoku Earthquake and its larger foreshocks and aftershocks
... The 2011 Tohoku Earthquake is the best-observed great earthquake, and it will undoubtedly become one of the most studied, owing both to its size and the enormous losses as- sociated directly ... See full document
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Ionospheric multiple stratifications and irregularities induced by the 2011 off the Pacific coast of Tohoku Earthquake
... strong earthquake with a magnitude of ...11, 2011, in ...height analysis of the ionograms showed a vertical structure with a scale size of 20∼30 ... See full document
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Initial 30 seconds of the 2011 off the Pacific coast of Tohoku Earthquake (Mw 9 0)—amplitude and τc for magnitude estimation for Earthquake Early Warning—
... and Dr. M. B¨ose and Professor K. Yomogida (editor), who gave useful comments for improving the manuscript. The waveform data are from K-NET and KiK-net of NIED. The hypocenter locations of the events are based on ... See full document
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Near field tsunami forecasting using offshore tsunami data from the 2011 off the Pacific coast of Tohoku Earthquake
... of data from the 2011 Tohoku ...at GPS buoys 802, 803, 804, and 806 ...sea surface around the epi- center ...northern Tohoku coastal region, the first peak amplitudes of the ... See full document
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The resonant response of the ionosphere imaged after the 2011 off the Pacific coast of Tohoku Earthquake
... of seismic and tsunami modes (with their energy mainly located in the solid Earth and ocean) and of atmospheric acoustic and gravity modes with their energy predominantly located in the atmosphere but related to a ... See full document
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Seismicity near the hypocenter of the 2011 off the Pacific coast of Tohoku earthquake deduced by using ocean bottom seismographic data
... and off-shore pas- sive seismic observation ...the earthquake epicen- ter was smaller than 200 km; (2) earthquakes whose epi- central distance to the nearest station was smaller than 40 km; and (3) ... See full document
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Aftershock observation of the 2011 off the Pacific coast of Tohoku Earthquake by using ocean bottom seismometer network
... Hypocenters were determined by the maximum- likelihood estimation technique of Hirata and Matsu’ura (1987). Due to uncertainty of the thickness of the sed- imentary layer and seismic velocity in the sedimentary ... See full document
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Numerical simulations of atmospheric waves excited by the 2011 off the Pacific coast of Tohoku Earthquake
... Figure 1 shows the observed TEC oscillations from 05:46 to 07:46 UT at 37.5 ◦ N, the same latitude as the ionospheric epicenter (see Tsugawa et al., 2011 for details). The TEC data are detrended with a ... See full document
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