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Some parts of Italy have a climate which cannot be precisely defined as either Cfa or Csa, presenting elements from both. This zone can be found both in some lake and hill resorts of Northern Italy (usually with wetter summers) and in some area like inner Tuscany (usually with drier summers). Florence is a good example of this transition climate:
Bolzano (Italian: [bolˈtsaːno] ⓘ or [bolˈdzaːno]; German: Bozen [ˈboːtsn̩] ⓘ; Ladin: Balsan or Bulsan) is the capital city of South Tyrol (officially the province of Bolzano), Northern Italy. With a population of 108,245, Bolzano is also by far the largest city in South Tyrol and the third largest in historical Tyrol.
The Köppen climate classification system was modified further within the Trewartha climate classification system in 1966 (revised in 1980). The Trewartha system sought to create a more refined middle latitude climate zone, which was one of the criticisms of the Köppen system (the climate group C was too general). [10]: 200–1
A map from 1874 showing South Tirol with approximately the borders of today's South and East Tyrol. South Tyrol (occasionally South Tirol) is the term most commonly used in English for the province, [10] and its usage reflects that it was created from a portion of the southern part of the historic County of Tyrol, a former state of the Holy Roman Empire and crown land of the Austrian Empire of ...
Ponte a Bozzone, Tuscany, Italy Tabernas Desert in Andalusia, Spain. The southern region of the European Union is mostly impacted by the Mediterranean Sea.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.
Today, the most commonly used climate map is the Köppen climate classification, developed by Russian climatologist of German descent and amateur botanist Wladimir Köppen (1846–1940), which divides the world into five major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature.
Climate classifications are systems that categorize the world's climates. A climate classification may correlate closely with a biome classification, as climate is a major influence on life in a region. The most used is the Köppen climate classification scheme first developed in 1884.
The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, location, and latitude.The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.