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Average annual temperatures in Greece range from around +4 °C (39 °F) in Kaimaktsalan up to +22 °C (72 °F) [8] in Lindos. The lowest average annual precipitation is recorded in Schoinoussa with 239 mm while the highest is found in Theodoriana with 2,529 mm. [ 7 ] The highest temperature ever recorded was 48.0 °C (118.4 °F) in Tatoi and ...
Average sea temperature °C (°F) 16.0 (61.0) 15.0 (59.0) 15.0 (59.0) 16.0 (61.0) ... This page was last edited on 30 October 2024, ... Greece. 8 languages ...
The Pagasetic Gulf (Greek: Παγασητικός Κόλπος, romanized: Pagasitikós Kólpos) is a rounded gulf (max. depth 102 metres) in the Magnesia regional unit (east central Greece) that is formed by the Mount Pelion peninsula. It is connected with the Euboic Sea. The passage into the Euboic Sea is narrow and is about 4 km.
A Mediterranean climate (/ ˌ m ɛ d ɪ t ə ˈ r eɪ n i ən / MED-ih-tə-RAY-nee-ən), also called a dry summer climate, described by Köppen and Trewartha as Cs, is a temperate climate type that occurs in the lower mid-latitudes (normally 30 to 44 north and south latitude).
Winter is the wet season and summers are hot and dry. The absolute maximum temperature on record is 40 °C (104 °F) in June and the absolute minimum in December is 0 °C (32 °F). Wind speed varies between 56 km/h (16 m/s; 35 mph) in August and 98 km/h (27 m/s; 61 mph) in October and February. [16]
The highest extreme temperatures have been recorded in Syracuse, Italy, with 48.8 °C (119.8 °F), [13] Athens and Elefsina, Greece, with 48.0 °C (118.4 °F) [14] and inside the southern valleys of the Iberian Peninsula, with towns such as La Rambla, Cordoba (Spain) and Amareleja (Portugal) recording temperatures of 47.6 °C (117.7 °F) [15 ...
Graph showing ocean temperature versus depth on the vertical axis. The graph shows several thermoclines (or thermal layers) based on seasons and latitude. The temperature at zero depth is the sea surface temperature. The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats.
The dense Mediterranean water sinks below the Black Sea inflow to a depth of 23–30 metres (75–98 ft), then flows through the Dardanelles Strait and into the Sea of Marmara at velocities of 5–15 cm/s (2–6 in/s). The Black Sea outflow moves westward along the northern Aegean Sea, then flows southwards along the east coast of Greece. [10]