BibSonomy publications for /author/KanamoriFri Feb 10 00:00:00 CET 2012IEEE Transactions on Information Theory2708-720$f$ -Divergence Estimation and Two-Sample Homogeneity Test Under Semiparametric Density-Ratio Models.582012dblp Thu Feb 02 00:00:00 CET 2012J. Optimization Theory and Applications1171-197Worst-Case Violation of Sampled Convex Programs for Optimization with Uncertainty.1522012dblp Wed Jan 25 22:41:56 CET 2012Physics Today1233+Insights from the great 2011 {Japan} earthquake642011earthquake geophysics seismology tohoku {The diverse set of waves generated in Earth's interior, oceans, and atmosphere during the devastating Tohoku-oki earthquake reveal some extraordinary geophysics.}Fri Jan 13 00:00:00 CET 2012IEICE Transactions123498-3504A Dynamic Spectrum Assignment Method for Call Blocking Probability Reduction in WiFi/WiMAX Integrated Networks.94-B2011dblp Sat Dec 17 01:41:12 CET 2011Naturefeb6567708--711The origin of harmonic tremor at {Old Faithful} geyser3791996geophysics seismology volcanoes 22{Volcanic eruptions are sometimes accompanied by a characteristic type of seismicity known as harmonic tremor, in which the signal is dominated by discrete vibration frequencies. This harmonic structure could reflect resonance behaviour in the excitation source or filtering of the seismic waves as they propagate through the surrounding rocks but complexity and variability in the properties of volcanic systems make it difficult to discriminate between such mechanisms. To address this question, we have analysed the source and propagation characteristics of seismicity at Old Faithful geyser (Yellowstone National Park), the cyclic behaviour and accessibility of which make it an ideal natural laboratory for studying harmonic tremor associated with near-surface sources. We find that sharp pressure pulses inside the water column trigger distinct seismic events that give rise to a harmonic ground response whose frequency varies spatially but not temporally. A superposition of these seismic events creates the appearance of continuous harmonic tremor. The absence of resonance within the water column suggests that the harmonic motion must arise from the interaction of the seismic waves with heterogeneities in the surrounding elastic medium-most probably a near-surface soft layer.}Mon Dec 05 00:00:00 CET 2011CoRRQuantum Three-Pass protocol: Key distribution using quantum superposition statesabs/1004.05992010dblp Thu Dec 01 00:00:00 CET 2011J. Log. Program.1&21-30Abstract Interpretation based on OLDT Resolution.151993dblp Thu Dec 01 00:00:00 CET 2011J. Log. Program.1&231-54Abstract Interpretation Based on Alexander Templates.151993dblp Fri Nov 25 00:00:00 CET 2011Encyclopedia of Complexity and Systems Sciencereference/complexity/20099577-9592Tsunami Earthquakes.2009dblp Thu Nov 17 00:00:00 CET 2011Neural Computation71437-1481Information Geometry of U-Boost and Bregman Divergence.162004dblp Thu Nov 17 00:00:00 CET 2011Neural Computation102469-2496Robust Regression with Asymmetric Heavy-Tail Noise Distributions.142002dblp Mon Nov 14 00:00:00 CET 2011Electr. Notes Theor. Comput. Sci.77-87Modular Modelling in Synthetic Biology: Light-Based Communication in E. coli.2772011dblp Mon Nov 07 00:00:00 CET 2011MIGconf/mig/2011192-203Lecture Notes in Computer ScienceTwisting, Tearing and Flicking Effects in String Animations.70602011dblp Fri Nov 04 13:47:04 CET 2011J. Appl. Polym. Sci.APR 1521465 -- 1470Mineralization of hydroxyapatite on a polymer substrate in a solution supersaturated by polyelectrolyte1002006imported Fri Nov 04 00:00:00 CET 2011IEICE Transactions101924-1932Multiscale Bagging and Its Applications.94-D2011dblp Fri Nov 04 00:00:00 CET 2011CASEconf/case/2010798-803Anti-windup controller design using gravity compensation for Euler-Lagrange systems with actuator saturation.2010dblp Tue Oct 25 00:00:00 CEST 2011CASEconf/case/2011798-803Global stabilization of anti-windup PID position control for euler-lagrange systems with actuator saturation.2011dblp Sun Sep 25 14:14:42 CEST 2011Geophysical Research Letterssep17L17308+Structural heterogeneity in the megathrust zone and mechanism of the 2011 {Tohoku-oki }earthquake ({Mw} 9.0)382011earthquake geophysics seismology subduction tohoku tomography 7{The great 2011 Tohoku-oki earthquake (Mw 9.0) and its 339 foreshocks and 5,609 aftershocks (9-27 March 2011) were relocated using a three-dimensional seismic velocity model and local P and S wave arrival times. The distribution of relocated hypocenters was compared with a tomographic image of the Northeast Japan forearc. The comparison indicates that the rupture nucleation of the largest events in the Tohoku-oki sequence, including the mainshock, was controlled by structural heterogeneities in the megathrust zone.}Sun Sep 25 14:14:42 CEST 2011Earth and Planetary Science Lettersaug3-4277--283Initiation of the great {Mw 9.0 Tohoku-Oki} earthquake3082011earthquake geophysics seismology source subduction tohoku {We determined the location, size, mechanism, and the frequency content of the first 4.0 s of the 2011 Tohoku-Oki earthquake. Since the beginning of this earthquake is very small, we develop a comparative approach against a near-by reference earthquake, the master event. We first determined the water depth near the master event using the differential timing between the water phase pwP reflected from the air-water interface and the depth phase pP reflected from the water-crust interface. Then we located the master event using the well-known ocean bathymetry in the area. After calibrating teleseismic arrays (D = 30 to 90 deg) at short periods for timing and amplitude with respect to the master event, we were able to determine the initiation of the main event. It began as a small (Mw = 4.9) thrust event located at 38.19N, 142.68E at a depth of 21 km, and, a few seconds later, evolved into a slower extremely large slip event up-dip.}Wed Sep 14 00:00:00 CEST 2011Parallel Computing3269-293Several partitioning strategies for parallel image convolution in a network of heterogeneous workstations.272001dblp