Automatic Feature Highlighting in Noisy RES Data With CycleGAN
Radio echo sounding (RES) is a common technique used in subsurface glacial imaging, which provides insight into the underlying rock and ice. However, systematic noise is introduced into the data during collection, complicating interpretation of the results. Researchers most often use a combination o...
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Zusammenfassung: | Radio echo sounding (RES) is a common technique used in subsurface glacial
imaging, which provides insight into the underlying rock and ice. However,
systematic noise is introduced into the data during collection, complicating
interpretation of the results. Researchers most often use a combination of
manual interpretation and filtering techniques to denoise data; however, these
processes are time intensive and inconsistent. Fully Convolutional Networks
have been proposed as an automated alternative to identify layer boundaries in
radargrams. However, they require high-quality manually processed training data
and struggle to interpolate data in noisy samples (Varshney et al. 2020).
Herein, the authors propose a GAN based model to interpolate layer boundaries
through noise and highlight layers in two-dimensional glacial RES data. In
real-world noisy images, filtering often results in loss of data such that
interpolating layer boundaries is nearly impossible. Furthermore, traditional
machine learning approaches are not suited to this task because of the lack of
paired data, so we employ an unpaired image-to-image translation model. For
this model, we create a synthetic dataset to represent the domain of images
with clear, highlighted layers and use an existing real-world RES dataset as
our noisy domain.
We implement a CycleGAN trained on these two domains to highlight layers in
noisy images that can interpolate effectively without significant loss of
structure or fidelity. Though the current implementation is not a perfect
solution, the model clearly highlights layers in noisy data and allows
researchers to determine layer size and position without mathematical
filtering, manual processing, or ground-truth images for training. This is
significant because clean images generated by our model enable subsurface
researchers to determine glacial layer thickness more efficiently. |
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DOI: | 10.48550/arxiv.2108.11283 |