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F. Crespon

Researcher at IPG Photonics

Publications -  7
Citations -  329

F. Crespon is an academic researcher from IPG Photonics. The author has contributed to research in topics: Rayleigh wave & Seismic wave. The author has an hindex of 6, co-authored 7 publications receiving 305 citations. Previous affiliations of F. Crespon include Paris Diderot University & Institut de Physique du Globe de Paris.

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Ground-based GPS imaging of ionospheric post-seismic signal

TL;DR: In this article, a continuous global positioning system (GPS) ionospheric tomography above Europe, Japan and California will be performed with the Service and Products of ionosphere Electronic Content and Tropospheric Refractive index over Europe (SPECTRE) experiment.
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Three-dimensional ionospheric tomography of post-seismic perturbations produced by the Denali earthquake from GPS data

TL;DR: In this article, a tomographic reconstruction of electron density perturbations in the acoustic frequency band is presented, with a timing consistent with an infrasonic wave generated by the path of seismic surface waves.
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Response of the ionosphere to the seismic trigerred acoustic waves: Electron density and electromagnetic fluctuations

TL;DR: In this article, the excitation of low-frequency (0001-10 Hz) electromagnetic and density fluctuations in the ionosphere during the passage of seismic triggered acoustic waves (AWs) was studied.
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Tsunami detection in the ionosphere

TL;DR: In this article, the authors presented some recent results regarding the detection of tsunami waves through perturbations induced in the ionosphere, which can be used to measure the sea surface variation in the case of large tsunamis.
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Seismic waves in the ionosphere

TL;DR: In this article, the authors proposed a method for remote detection of the seismic signals from space, which is based on the detection of very low ground displacements: even at the most noisy frequency, 0.15Hz, associated with a global seismic noise generated by the oceanic waves, the amplitude of the ground displacement noise is in the range of 0.1-10 micrometers and good signal to noise seismic waves have amplitudes of a hundred to a thousand times higher.