Denoised data for the manuscript "Self-Supervised Coherence-Based Denoising of Cryoseismological Distributed Acoustic Sensing Data"

These datasets provide the necessary data to reproduce the results presented in the paper “Self-Supervised Coherence-Based Denoising of Cryoseismological Distributed Acoustic Sensing Data.” The corresponding code is available on GitHub, and the paper can be accessed via Authorea.

The data set "02_accumulation_denoisedDAS" contains the denoised data of the model J-invariant-cryo-acc.
The data sets , "11_vanende_earth_denoisedDAS_image", "12_vanende_finetuned_cryo_denoisedDAS_image", "13_afk_denoisedDAS_image", "14_conventional_denoisedDAS_image", and "15_DASDL_denoisedDAS_image" contain the some denoised data files for the models "J-invariant-earth", "J-invariant-earth-cryo", ""AFK", "Conventional", and "DASDL" , needed for reproducing Figure 5, S7, and S8.

Abstract:

A major challenge in cryoseismology is that signals of interest are often buried within the high noise level emitted by a variety of environmental processes. Particular Distributed Acoustic Sensing (DAS) data often suffers from low signal-to-noise ratios (SNR) potentially resulting in a multitude of undetected events of interest, which further remain unanalyzed. To record seismicity, we deployed a DAS system on Rhône Glacier, Switzerland, using a 9 km long fiber-optic cable that covered the entire glacier, from its accumulation to its ablation zone. The highly active and dynamic cryospheric environment, in combination with poor coupling, resulted in DAS data characterized by a low SNR. Our objective is to develop and evaluate a method to effectively denoise this cryoseismological DAS dataset, while comparing our approach to state-of-the-art filtering and denoising methods. We propose the J-invariant-cryo denoiser, specifically trained on cryoseismological data and capable of separating incoherent environmental noise from temporally and spatially coherent signals of interest, based on a self-supervised J-invariant U-Net autoencoder. The method enhances inter-channel coherence, improves waveform similarity with co-located seismometers, and increases SNR. The comparison of different methods shows that our approach obtains the highest gain in SNR and highest similarity with co-located seismometers, while suffering from denoising artifacts in rare cases. The proposed denoiser has the potential to enhance the detection capabilities of events of interest in cryoseismological DAS data, hence to improve the understanding of processes within Alpine glaciers.