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Annual precipitation averages about 635 mm (25 in) in central Transylvania, 521 mm (20.5 in) at Iaşi in Moldavia, and only 381 mm (15 in) at Constanţa on the Black Sea. Romania map of Köppen climate classification, according to Clima României from the Administrația Națională de Meteorologie , Bucharest 2008
Dubrovnik has a Mediterranean climate (Köppen: Csa). Dubrovnik has hot, muggy, relatively dry summers and mild to cool wet winters. The bora wind blows cold gusts down the Adriatic coast between October and April, and thundery conditions are common year round, even in summer, when they interrupt the warm, sunny days. The air temperatures can ...
The list of snowiest places in the United States by state shows average annual snowfall totals for the period from mid-1985 to mid-2015. Only places in the official climate database of the National Weather Service, a service of NOAA, are included in this list. Some ski resorts and unofficial weather stations report higher amounts of snowfall ...
The average high temperature in Boise at the start of September is 86 degrees — but the city has already hit or exceeded 100 degrees four times this month, reaching 104 degrees on Wednesday ...
Srđ is a low mountain just behind the walled city of Dubrovnik in Dalmatia, Croatia. [1] The mountain, part of the Dinaric Alps , has a height of 412 metres (1,352 ft). [ 2 ] At its top is a large white stone cross and Fort Imperial , a defensive structure built by the French in 1810 during the Napoleonic Wars .
The winter average varies from 6 °C (42.8 °F), in the northern areas, to 11–14 °C (51.8–57.2 °F) in the southern islands. During the summer, averages are near 23 °C (73.4 °F) in the north (Liguria) and sometimes reach 26–28 °C (78.8–82.4 °F) in the south. Precipitation mostly occurs during the winter.
The image above shows where average air temperatures (October 2010 – September 2011) were up to 3 degrees Celsius above (red) or below (blue) the long-term average (1981–2010). The map shows the 10-year average (2000–2009) global mean temperature anomaly relative to the 1951–1980 mean.
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