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  1. Hot-summer Mediterranean climate ( Csa) Warm-summer Mediterranean climate ( Csb) A Mediterranean climate ( / ˌmɛdɪtəˈreɪniən / MED-ih-tə-RAY-nee-ən ), also called a dry summer climate, described by Köppen as Cs, is a temperate climate type that occurs in the lower mid-latitudes (normally 30 to 44 north and south latitude).

  2. Das Csa-Klima – von Köppen auch „Olivenklima“ genannt, [3] englisch Hot-summer Mediterranean climate [4] (= Sommerheißes Mittelmeerklima) – grenzt im Wesentlichen die Kernbereiche der Klimate der subtropischen Hartlaubgebiete ein. a = Die Sommer sind heiß und schwül, der wärmste Monat liegt im Mittel über 22 °C.

  3. Csa = Hot-summer Mediterranean climate; coldest month averaging above 0 °C (32 °F) (or −3 °C (27 °F)), at least one month's average temperature above 22 °C (71.6 °F), and at least four months averaging above 10 °C (50 °F). At least three times as much precipitation in the wettest month of winter as in the driest month of ...

  4. Mediterranean climate. A Mediterranean climate is a climate that has dry summers that are mild to hot as well as winters that are mild to cool with moderate or high rainfall. It includes the climate of much of the land near the Mediterranean Sea.

  5. 11. Apr. 2024 · Mediterranean climate, major climate type of the Köppen classification characterized by hot, dry summers and cool, wet winters and located between about 30° and 45° latitude north and south of the Equator and on the western sides of the continents.