Recent studies have highlighted a potential correlation between climate change and increased seismic activity. Mechanisms such as glacial isostatic adjustment, sea-level rise, and hydrological changes are posited to influence tectonic stress fields, potentially triggering earthquakes. For instance, the melting of glaciers reduces overburden pressure, leading to crustal rebound and fault reactivation. Similarly, rising sea levels and altered precipitation patterns can modify pore pressures within fault zones. While these processes are theoretically plausible, the extent of their impact on seismicity remains a subject of ongoing research. I invite colleagues and experts to share their insights and recent findings on this topic. How do we quantify the influence of climatic factors on seismic hazards? What methodologies are being employed to disentangle anthropogenic effects from natural variability in seismic activity?