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Highest temperatures ever recorded in Spain [ edit ] On July 30, 1876 and August 4, 1881, temperatures of 51.0 °C (123.8 °F) and 50.0 °C (122.0 °F) [ 1 ] were both reported for Seville : these readings are unreliable, since they were measured under a standard exposure and in poor technical conditions. [ 2 ]
Because of the Foehn effect, the southern slopes fall inside the rain shadow zone and so Green Spain contrasts starkly with the rest of Spain. The rainfall is generally abundant, exceeding 1,000 mm (39.4 in) and is fairly evenly spread out over the year, with the driest month above 30 mm (1.2 in), which is the minimum criteria for an oceanic ...
The town of Chiva, west of Valencia province, recorded 491mm of rain in just eight hours – more than it has seen over the past 20 months, according to Spain’s weather service.
This is a list of cities by average temperature (monthly and yearly). The temperatures listed are averages of the daily highs and lows. Thus, the actual daytime temperature in a given month may be considerably higher than the temperature listed here, depending on how large the difference between daily highs and lows is.
However, the National Weather Service at Wilmington's records show the lowest wind chill value ever recorded was -48 degrees at Cincinnati/ Northern Kentucky International Airport in 1985. Those ...
Fuengirola (pronounced [fweŋxiˈɾola]) is a city on the Costa del Sol in the province of Málaga in the autonomous community of Andalusia in southern Spain.It is located on the central coast of the province and integrated into the region of the Costa del Sol and the Commonwealth of Municipalities of the Costa del Sol Occidental.
Christopher C. Burt, a weather historian writing for Weather Underground, believes that the 1913 Death Valley reading is "a myth", and is at least 2.2 or 2.8 °C (4 or 5 °F) too high. [13] Burt proposes that the highest reliably recorded temperature on Earth could still be at Death Valley, but is instead 54.0 °C (129.2 °F) recorded on 30 ...
Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and 45 degrees north or south of the equator. The main cause of Mediterranean, or dry summer, climate is the subtropical ridge , which extends towards the pole of the hemisphere in question during the summer and migrates towards the ...