Travel time: Year-round
Genoa (Genova) possesses a unique Mediterranean climate influenced heavily by its dramatic geography—wedged between the Ligurian Sea and the steep Apennine Mountains. This vertical landscape creates significant weather variations within just a few kilometers, making it one of the most climatically interesting cities in Italy.
Genoa is known for its mild, temperate conditions but also for being the rainiest major city in Italy. Because the mountains rise directly behind the coast, they trap humid air moving in from the sea, leading to frequent aesthetic or heavy rainfall. While winters are rarely freezing and summers are rarely scorching, the city experiences high humidity year-round.
A weather phenomenon specific to Genoa and Liguria is the Maccaia. This occurs when a warm, humid south wind (the Scirocco) meets a cooler sea surface, creating a low-lying, thick layer of gray clouds that hugs the coast. Even in spring or summer, the Maccaia can turn a bright day gray and humid in minutes, though it rarely produces rain. It creates a melancholic, "heavy" atmosphere that is a staple of local literature and mood.
Genoa’s climate varies dramatically with elevation. While the coastal neighborhoods (Boccadasse or Nervi) might be enjoying a sunny 12°C in January, the upper residential districts like Righi or Quezzi, just a 15-minute funicular ride up, can be shrouded in fog or experiencing light sleet. The western part of the city (Ponente) is often windier and slightly cooler than the eastern side (Levante).
Locals define their days by the wind:
Historically, Genoa’s architecture—tall buildings and narrow alleys called Caruggi—acts as a natural climate control system. These deep stone canyons remain cool during the humid summer heat and provide shelter from the lashing autumn rains and the biting winter Tramontana. Locals are deeply attuned to the "Sea State"; the city has a long history of maritime weather monitoring, and residents are quick to adapt, moving from beachfront promenades to protected interior squares at the first sign of a shift in the wind.