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Climate of Italy

  • 16 min read
  • 9 chapters

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Through Rome, Europe and Sea level rise

Between the north and south, there can be a considerable difference in temperature, especially during in winter: on some winter days, it can be −2 °C (28 °F) and snowing in Milan, while it is 8 °C (46.4 °F) in Rome and 20 °C (68 °F) in Palermo. Temperature differences are less extreme in the summer. On 11 August 2021, an agricultural monitoring station near Syracuse recorded 48.8 °C (119.8 °F) which constitutes the official record for the highest temperature in Europe according to the World Meteorological Organization.

Italy is experiencing widespread impacts of climate change, with an increase in extreme events such as thunderstorms heatwaves, droughts and more frequent flooding. For example, Venice is facing increasing issues due to sea level rise. Italy faces many challenges adapting to climate change including the economic, social, and environmental impacts that climate change creates, as well as an increasingly problematic death toll from the health risks that come with climate change.

Generality

The Italian climate is influenced by the Mediterranean Sea, a large body of water that surrounds Italy on every side except the north. This sea constitutes a reservoir of heat and humidity for Italy. Within the southern temperate zone, they determine a Mediterranean climate with local differences due to the geomorphology of the territory, which tends to make its mitigating effects felt, especially in high pressure conditions.

In addition to Mediterranean influences, the Italian climate is partly affected by the western currents, especially in the intermediate seasons, as well as by the dynamics in the Atlantic Ocean, with its cyclones that travel from west by the reciprocal position, on a synoptic level, of the Azores anticyclone and the African subtropical anticyclone. The cold winter air are in part influenced by the mountain ranges of the Alps and the Apennines. The mitigating effect of the Mediterranean is added to this condition, with a tendency to reinvigorate, due to the transfer of sensible heat and humidity, the weakened perturbations from the west or with the formation of Mediterranean Low or Mediterranean cyclogenesis.

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