This study analyzes the climatology of Large Scale Traveling Ionospheric Disturbances (LSTIDs) over Europe from 2014 to 2023 using the HF-Interferometry method (HF-INT), which provides LSTID's activity detected in near-real-time by a network of European ionosondes. For this purpose, this LSTID activity has been analyzed in depth and a Catalogue of observed LSTID events has been obtained providing, among others, the onset time, duration, dominant period, and propagation velocity vector of each LSTID event. The results, derived from this Catalogue of LSTIDs, reveal that LSTID occurrence is significantly dependent on local time, seasonal variations, and geomagnetic conditions, with activity peaks observed during equinoxes, particularly at night and in the early morning hours. Key propagation characteristics include velocities ranging from 500 to 700 m/s and azimuths, suggesting a southward direction, closely associated with auroral activity. Additionally, a distinct westward propagation in the morning hours is attributed to the solar terminator effect. These findings highlight the complex interactions between ionospheric dynamics and geomagnetic conditions, offering new insights into the mechanisms governing TID generation and propagation.