The ambient seismic field at Valhall contains omnidirectional noise suitable for seismic noise
tomography at low frequencies between 0.35 Hz and 1.75 Hz. Scholte-waves traveling along the
ocean floor can provide a tomographic image of features in the near surface (between 0 and 105
meters beneath the ocean floor). We have demonstrated that eikonal
tomography is an effective tool for studying surface waves at Valhall, even though the gradient estimate sets
do not closely resemble Gaussian distributions. This research shows that there is potential for developing a
low-cost near-surface monitoring system using passive noise recorded by permanent ocean-bottom
arrays.