Whether acoustic, elastic, or electromagnetic, waves can be used to probe for information about an unknown medium. In the first step of the probe, transducers in acoustics, seismographs in geophysics, or antennas in electromagnetics generate waves, and an array of receivers records them. In the second numerical step, the recorded data is processed in order to estimate some relevant features of the medium : source or reflector locations and shapes.
When only rough forward models, and limited and noisy data are available, the challenge is to estimate parts of the unknown structure. The whole process consists in detecting and localizing sources and reflectors in order to reconstruct small inclusions and shape deformations.
A breakthrough by the introduction of cross correlations in the noughties have led to a distinctive approach to imaging. This finding originated from unexpected consequences observed in time reversal experiments. Recording waves by a network of receivers and regenerating them into the medium after time reversal, made it possible to focus the waves on the original sources, or on reflectors. Surprisingly, refocusing the waves in a randomly perturbed medium worked much better than it did in a homogeneous one.
In multistatic imaging, the central issue is to quantify and understand the trade-offs between data size, computational complexity, signal-to-noise ratio, and resolution. The trade-off between resolution and stability is critical when the data are noisy. Noise may appear in different forms in multistatic imaging. The receivers may be responsible for measurement noise, meaning the recorded data are corrupted by additive and uncorrelated noise. This type of noise is well understood and can be mitigated by classical imaging functions, such as least-square imaging (or full waveform inversion), reverse-time migration or travel-time migration.
The medium can be responsible for noise. The background medium can be heterogeneous, and scattering then produces clutter noise in the data. Clutter noise has a very different structure compared to measurement noise because of its nontrivial correlation properties. Sivienn analyzes the correlations of the recorded signals that carry information about the medium.
The sources can be responsible for noise. They may be imperfectly controlled. Nevertheless, uncontrolled or even ambient noise sources can generate waves that carry information about the medium in their correlations. Sivienn's original approach is to analyze the correlations of the recorded signals and to extract the information contained in them.
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