Venice flooding is caused by a combination of Adriatic tidal cycles, southerly sirocco winds, and low atmospheric pressure pushing seawater into the lagoon. The MOSE barrier system, operational since 2020, now prevents the most severe events, though moderate flooding still occurs during the October-to-March season. The historic low point is Piazza San Marco, which begins to flood at just 80 cm above the standard tidal datum. At 110 cm, roughly 12% of the city goes underwater. At 130 cm, nearly 70% is submerged. The catastrophic flood of November 2019 reached 187 cm, the worst event since 1966 and a stark reminder of the city's vulnerability. Italy's answer to this ongoing threat is MOSE (Modulo Sperimentale Elettromeccanico), a massive flood barrier system spanning the three inlets that connect the Adriatic to the Venetian lagoon: Lido, Malamocco, and Chioggia. Construction began in 2003 and the system became operational in 2020 after years of delays and cost overruns. When tides are forecast to exceed 110 cm, 78 hinged steel gates rise from the seabed to temporarily seal off the lagoon. MOSE has already prevented multiple flooding events that would have otherwise inundated the city. The Centro Previsioni e Segnalazioni Maree (the city's tide forecasting centre) monitors conditions continuously and issues alerts via its website, a Telegram channel, and a siren system throughout the city. Visitors can check real-time tide data and forecasts before planning their day. The flooding season runs primarily from October through March, with November and December historically seeing the highest tides.