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With the exception of Madrid, [9] Lisbon [10] and Athens, [11] Rome has the highest UV index between European capitals (only in the continent) and values close to that of Chicago at 41.9 °N as ultraviolet radiation is less interfered with by other geographic variables, but with a moderate annual average with index equal to 5, which allows ...
Rome has a Mediterranean climate (Köppen climate classification: Csa), [76] with hot, dry summers and mild, humid winters. Its average annual temperature is above 21 °C (70 °F) during the day and 9 °C (48 °F) at night.
Because most regions with a Mediterranean climate are near large bodies of water, temperatures are generally moderate, with a comparatively small range of temperatures between the winter low and summer high unlike (the relatively rare) dry-summer humid continental climates (although the daily diurnal range of temperature during the summer is ...
A relatively "continental" and "four-season" version of the humid subtropical climate can be found in the Po and Adige valleys in the North, and sometimes in low inland Central and Southern Italy. It is marked by hot and wet summers, while winters are moderately cold. The precipitation is higher and there is no dry season.
The climate of ancient Rome varied throughout the existence of that civilization. In the first half of the 1st millennium BC, the climate of Italy was more humid and cool than now and the presently arid south saw more precipitation . [ 1 ]
Unlike the dry summer Mediterranean climates, humid subtropical climates have a warm and wet flow from the tropics that creates warm and moist conditions in the summer months. As such, summer (not winter as is the case in Mediterranean climates) is often the wettest season.
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Water temperatures there are mild in winter and warm in summer and give name to the Mediterranean climate type due to the majority of precipitation falling in the cooler months. During the summer, the weather is most frequently sunny and dry, and any precipitation falls in the form of showers or thunderstorms from cumuliform clouds.