102 research outputs found
Seismic-phase detection using multiple deep learning models for global and local representations of waveforms
The detection of earthquakes is a fundamental prerequisite for seismology and
contributes to various research areas, such as forecasting earthquakes and
understanding the crust/mantle structure. Recent advances in machine learning
technologies have enabled the automatic detection of earthquakes from waveform
data. In particular, various state-of-the-art deep-learning methods have been
applied to this endeavour. In this study, we proposed and tested a novel phase
detection method employing deep learning, which is based on a standard
convolutional neural network in a new framework. The novelty of the proposed
method is its separate explicit learning strategy for global and local
representations of waveforms, which enhances its robustness and flexibility.
Prior to modelling the proposed method, we identified local representations of
the waveform by the multiple clustering of waveforms, in which the data points
were optimally partitioned. Based on this result, we considered a global
representation and two local representations of the waveform. Subsequently,
different phase detection models were trained for each global and local
representation. For a new waveform, the overall phase probability was evaluated
as a product of the phase probabilities of each model. This additional
information on local representations makes the proposed method robust to noise,
which is demonstrated by its application to the test data. Furthermore, an
application to seismic swarm data demonstrated the robust performance of the
proposed method compared with those of other deep learning methods. Finally, in
an application to low-frequency earthquakes, we demonstrated the flexibility of
the proposed method, which is readily adaptable for the detection of
low-frequency earthquakes by retraining only a local model
細胞内における遺伝子制御ネットワークの解明を目的とした粒子フィルタとMCMCによるハイブリッド版パラメータ推定法の開発
Open House, ISM in Tachikawa, 2010.7.9統計数理研究所オープンハウス(立川)、H22.7.9ポスター発
線虫細胞内における細胞質流動のデータ同化研究
Open House, ISM in Tachikawa, 2012.6.15統計数理研究所オープンハウス(立川)、H24.6.15ポスター発
Experimental characterization of the electronic structure of anatase TiO2: Thermopower modulation
Thermopower (S) for anatase TiO2 epitaxial films (n3D: 1E17-1E21 /cm3) and
the gate voltage (Vg) dependence of S for thin film transistors (TFTs) based on
TiO2 films were investigated to clarify the electronic density of states (DOS)
around the conduction band bottom. The slope of the |S|-log n3D plots was -20
{\mu}V/K, which is an order magnitude smaller than that of semiconductors (-198
{\mu}V/K), and the |S| values for the TFTs increased with Vg in the low Vg
region, suggesting that the extra tail states are hybridized with the original
conduction band bottom.Comment: 11 pages, 4 figure
Adjoint-based uncertainty quantification for inhomogeneous friction on a slow-slipping fault
Long-term slow-slip events (LSSEs) usually occur on the deep, shallow parts
of subducting plates and have substantial relation with adjacent megathrust
fault motion. Conventional techniques of quantifying slow earthquake frictional
features show that these features may be indicative of predictive seismic
motion; however, quantifying high-accuracy uncertainty of the frictional fields
has not yet been achieved. We therefore propose a method of uncertainty
quantification for spatially inhomogeneous frictional features from slip motion
on an LSSE fault--megathrust fault complex in southwestern Japan. By combining
a fault motion model that mimics slow-slip motion and a variational data
assimilation (DA) technique using a second-order adjoint method, we have
succeeded in quantifying the spatial distribution of the uncertainty of the
frictional features. Further, evaluation of the spatial distribution in
high-resolution reveals the correlation between the dynamics of the slow-slip
motion and the important components of the frictional features, which is
valuable information for observational DA design. Findings from this study are
expected to advance the theoretical foundation of applied seismic motion
prediction techniques using slow-slip frictional features as stress meters for
megaquakes, as well as improve understanding of the relationship between the
slow-slip motion and frictional parameters of a fault
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