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Ponte a Bozzone, Tuscany, Italy Tabernas Desert in Andalusia, Spain. The southern region of the European Union is mostly impacted by the Mediterranean Sea.Water temperatures there are mild in winter and warm in summer and give name to the Mediterranean climate type due to the majority of precipitation falling in the cooler months.
An image of the Gulf Stream's path and its related branches The average number of days per year with precipitation The average amount of sunshine yearly (hours). The climate of western Europe is strongly conditioned by the Gulf Stream, which keeps mild air (for the latitude) over Northwestern Europe in the winter months, especially in Ireland, the United Kingdom and coastal Norway.
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.
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This is a list of countries and sovereign states by temperature.. Average yearly temperature is calculated by averaging the minimum and maximum daily temperatures in the country, averaged for the years 1991 – 2020, from World Bank Group, derived from raw gridded climatologies from the Climatic Research Unit.
Sunshine hours for selected cities in Europe Country City Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Ref. Albania: Tirana: 124 125 165 191 263 298 354 327 264 218 127 88 2,544 [1] Albania: Vlorë: 133 148 173 225 273 318 369 344 279 211 117 99 2,690 [2] [3] Albania: Durrës: 133 135 173 207 279 318 375 325 261 217 147 124 2,696 ...
Americans are crowding into Europe’s travel hot spots. Here are the less-crowded places where Europeans are going instead. Americans are flocking to Europe’s hot spots.
Diablo (hot, dry, offshore wind from the northeast in the San Francisco bay) The Hawk (cold winter wind in Chicago) Jarbo Gap Wind (associated with and often referred to as a Diablo Wind; katabatic winds in the Northern Sierra Nevada in the vicinity of Jarbo Gap, often contributing to the growth of local wildfires) [8] [9]