London Clay, which underlies the majority of Greater London, has a high shrink-swell potential that can result in damage to foundations and surface infrastructure due to seasonal expansion and contraction of the clay. Currently, surface movement as a result of shrink-swell is not monitored in London, meaning that the magnitude and cyclicity of these movements is poorly understood. Persistent Scatterer Interferometric Synthetic Aperture Radar (PSI) data provide highprecision line-of-sight displacement measurements at a high point density across urban areas,