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The Köppen classification has been the nice acknowledged and maximum used weather classification system for more than 70 years.
Mediterranean climate, main weather sort of the köppen category characterized by means of warm, dry summers and cool, wet winters and placed among approximately 30° and 45° latitude north and south of the Equator and at the western aspects of the continents.
In the okayöppen climate category: type B climates. Arid and semiarid climates cover approximately a quarter of Earth's land floor, in most cases among 50° N and 50° S, however, they may be in particular determined in the 15–30° latitude belt in both hemispheres. They showcase low precipitation and remarkable variability in precipitation over the year.
There are dry weather types: arid and semiarid. maximum arid climates acquire 10 to 30 centimeters (4 to 12 inches) of rain each yr, and semiarid climates acquire sufficient to support sizable grasslands. Temperatures in both arid and semiarid climates display massive everyday and seasonal variations.
The earliest recognized category of climate, devised by means of the Greeks, without a doubt divided every hemisphere right into a mathematical climate of 3 zones, the "summerless," "intermediate," and "winterless," as a consequence accounting handiest for the latitudinal variations in sun impact (the Greek word Klima method "inclination").
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