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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. Spain is the most climatically diverse country in Europe with 13 different Köppen climates. [1] [2] [3] The four most dominant climates in the country include: The hot-summer Mediterranean climate ( Csa ), the warm-summer Mediterranean climate ( Csb ), the steppe climate ( BSh and BSk) and the oceanic climate ( Cfb ).

  4. 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 ...

  5. Warm-summer Mediterranean climate (Csb) exists in roughly the same areas but in higher elevations (>1,000 m.), such as mount Parnitha in Attica. Climate data for Downtown Athens (1991–2020), Extremes (1890–present)