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- 2013–2014 Atlantic winter storms in Europe were a series of winter storms affecting areas of Atlantic Europe and beyond. The French Atlantic coastal regions (chiefly Brittany), South West and Southern England, West Wales, Ireland, Spanish Atlantic coastal regions (particularly Galicia) were especially affected by a "conveyor belt" series of high-precipitation storms (mostly not exceptional for their winds) and by high tides. Many storms were explosively deepened by a strong jet stream, many deepening below 950 hPa. The repeated formation of large deep lows over the Atlantic brought storm surges and large waves which coincided with some of the highest astronomical tides of the year and caused coastal damage. The low pressure areas brought heavy rainfalls which led to flooding, which became most severe over parts of England such as at the Somerset Levels. The repeated storms fit into a pattern of disturbed weather in the Northern Hemisphere, which saw from November 2013 a disturbance to the jet stream in the western Pacific, which propagated eastwards bringing a warm winter to Alaska, drought to California, and repeated cold air outbreaks to the eastern USA where the early 2014 North American cold wave resulted. (en)
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- 23538 (xsd:nonNegativeInteger)
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- NOAA North Atlantic wind speed anomaly January–February 2014 (en)
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- 2013-12-21 (xsd:date)
- 2013-12-28 (xsd:date)
- 2014-01-01 (xsd:date)
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- 2013-12-17 (xsd:date)
- 2013-12-21 (xsd:date)
- 2013-12-25 (xsd:date)
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- 2013 (xsd:integer)
- Erich (en)
- Dirk (en)
- Bernd (en)
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- European windstorms (en)
- Extratropical cyclones (en)
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- 2013–2014 Atlantic winter storms in Europe were a series of winter storms affecting areas of Atlantic Europe and beyond. The French Atlantic coastal regions (chiefly Brittany), South West and Southern England, West Wales, Ireland, Spanish Atlantic coastal regions (particularly Galicia) were especially affected by a "conveyor belt" series of high-precipitation storms (mostly not exceptional for their winds) and by high tides. Many storms were explosively deepened by a strong jet stream, many deepening below 950 hPa. The repeated formation of large deep lows over the Atlantic brought storm surges and large waves which coincided with some of the highest astronomical tides of the year and caused coastal damage. The low pressure areas brought heavy rainfalls which led to flooding, which became (en)
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- 2013–2014 Atlantic winter storms in Europe (en)
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