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In Zagora, Greece, 29.68 inches (754 mm) of rain fell in a single day from the storm, setting a new 24-hour rainfall record for the entire country. That beats the old record of 25.38 inches (645 ...
As a result, there is also significant socio-economic threats to vulnerable populations around the world from flooding. [38] For example, in Bangladesh in 2007, a flood was responsible for the destruction of more than one million houses. And yearly in the United States, floods cause over $7 billion in damage. [39]
A flash flood in Canandaigua, New York in 2017, greatly inundates a small ditch, flooding barns and ripping out newly installed drain pipes. The United States National Weather Service gives the advice "Turn Around, Don't Drown" for flash floods; that is, it recommends that people get out of the area of a flash flood, rather than trying to cross ...
Here’s what else is happening related to extreme weather, climate and the environment right now: —The World Meteorological Organization announced another heat record in a year full of them ...
An example is the 2009 Red River Flood and the 2009 Alaska floods. The second type of hazard occurs as the ice jam breaks apart, and a sudden surge of water breaks through flooding areas downstream of the jam (see below). Such a surge occurred on the St. Lawrence River in 1848. [9]
"Dangerous conditions with a high risk of flash flooding, mudslides and other debris flows with washouts are likely." As of early Saturday local time, up to a foot of rain has fallen, with 6-10 ...
The 2009 Angola, Namibia and Zambia floods was a natural disaster which began in early March 2009 and resulted in the deaths of at least 131 people and otherwise affected around 445,000 people. The floods affected seven regions of Namibia, three provinces of Zambia, two regions of Angola and part of Botswana. The floodwaters damaged buildings ...
Coastal flooding during Hurricane Lili in 2002 on Louisiana Highway 1 (United States). Coastal flooding occurs when dry and low-lying land is submerged by seawater. [1] The range of a coastal flooding is a result of the elevation of floodwater that penetrates the inland which is controlled by the topography of the coastal land exposed to flooding.