Travel time: Year-round
The Amalfi Coast is defined by a classic Mediterranean climate, where the dramatic Lattari Mountains meet the Tyrrhenian Sea. This vertical landscape creates a unique meteorological environment that dictates the rhythm of life for both locals and travelers.
The region experiences four distinct phases. Summers are characterized by long, hot, and dry periods where the sun dominates the sky for roughly 13 hours a day. Winters bring the bulk of the annual rainfall, often arriving in intense but short-lived bursts influenced by the surrounding mountains. Transition seasons, Spring and Autumn, are famously mercurial; a brilliant sunny morning in Ravello can quickly transform into a misty afternoon as clouds roll off the peaks.
On a typical clear day, the coast follows a predictable thermal pattern:
The Amalfi Coast is not a meteorological monolith. Elevation is the primary driver of variation:
A specific phenomenon to the Amalfi Coast is the interaction of south-westerly winds. When a strong Libeccio or Scirocco (a hot, dusty wind from the Sahara) blows, it can create massive sea swells. Locals watch for "mareggiata"—spectacular displays where waves crash against the sea walls of Amalfi and Minori.
Historically, the weather dictated the agricultural calendar for the famous Sfusato Amalfitano lemons. Locals built "pagliai" (straw coverings) and later black nets to protect the trees from winter hailstorms and rare frosts. You will still see these structures today, a testament to the region's adaptation to its environment. During the quietest winter months (January–February), many residents choose to travel, as the damp cold and rough seas make the usually vibrant coastal villages feel "melancholy" and introspective.
In the summer, the weather is more than just a number; it is an immersive experience of light and heat reflecting off the Mediterranean. The air feels saline and thick with the smell of the sea. In the winter, the "chill" comes from the high humidity rather than freezing temperatures—a dampness that lingers in the stone corridors of the ancient towns.