Floods

Why The Flood Happened. The North sea, between Britain and northern nuclear number 63 has a long annals of pelter disasters. combined effect of coerce surge and high runs tide of 31 Jan 1953 was a full moon throttle tide, approach the equinox tide rooceante higher than expected because of atmospheric wring and wind intense stamp moving from the Atlantic, turning south east to the North Sea i of the most impetuous and prolonged northerly gales in British meteorological history tidal surge developed and moved take rectify east coast tide 8-9 ft above predicted take aims - intensity level of clinical depression sucks the sea to its centre surge of 31 Jan 1953 took 11 hours to travel from Aberdeen to the Thames estuary, construct progressively It happened in the darkness or early morning, February 1st, 1953. A north-western storm was blowing and it was to be spring tide. At low tide the weewee system level at sea was as high as it is normally when it is high tide.

Then the wind pushed the water up to leaven even higher and the sea reached a disc extremum of 4, 5 meter above mean sea level. In The Netherlands the dikes were breached at many places in the provinces along the south-western coast. Sea water covered large areas. Near the breaches houses were ruined by the commit of the water rushing in. Many people were caught unawares, thither was no warning system and people were sleeping. In the send absent there were 1.800 victims. About 72.000 people had to be evacuated. Roads were done for(p) and telephone lines were down. In large areas relief could only b e brought by boat. Many cattle died, crops f! ailed, buildings were ruined.If you want to get a full essay, order it on our website: OrderCustomPaper.com

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