Timișoara, in western Romania close to the Serbian and Hungarian borders, receives around 600 mm (about 24 inches) of rain a year, with a summer peak from convective storms typical of the flat Pannonian plain the city sits on. Without significant nearby terrain to trigger storms, summer convection depends heavily on daytime heating, meaning the most intense cells tend to build during the hottest afternoons. The Bega Canal running through the city has occasionally seen elevated levels during sustained heavy rain, though this is a comparatively modest risk. Because these storms can develop with only modest warning, radar tracking is a genuinely practical tool for the region’s agricultural community. Romania’s National Meteorological Administration operates the national radar network.
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