Storm Event

Floods cause weekend shoppers in Hull to flee in terror with many rescued from rooftops

Severity ? 4


The storm responsible for this event initiated west of Iceland at about 65o N on 15th December 1921, following an easterly path towards Scandinavia over the next two days. By 17th December, the storm had developed considerably with a central air pressure of approximately 960 mbar while centred over the Norwegian Sea. Strong north-westerly to northerly winds were present over the North Sea before the storm continued eastwards and dissipated over Europe (The Argus, 1921; Met Office, 1921).

Hickey (1997) described “unprecedented” high tides at Alloa (Scotland), which were the highest in a “considerable number of years”, and also reports a high tide of 10.4 ft. OD [3.17 m] at Aberdeen. Within the national tide gauge network, only the Newlyn tide gauge was operational at the time, but has missing data for this period. The event occurred at peak spring tides.

We are unaware of any sources of information that describe the wave conditions during this event.


We are unaware of any information regarding the flood defence pathways for this event. The most specific available information regarding inundation is that almost every business and public building in the old town was flooded up to 4 ft. [1.22 m], including the Town Hall, the Post Office, Holy Trinity Church, St. Mary’s Church, and the Bank of England (The Times, 1921). See below for some further details of inundation.

Receptor and Consequence

Despite the lack of detailed information, the few existing accounts of this event paint a harrowing picture. Several sources describe very dramatic flooding at Hull, where some streets were flooded to a depth of 8 ft. [2.44 m], with people hurriedly escaping to higher ground and many later rescued from upper-floor windows and rooftops (The Argus, 1921). Estimated damages at Hull totalled at £750,000 (equivalent to around £30 million in 2014 prices; The Argus, 1921). According to The The Times, 1921, the worst affected area was part of the Wincolmlee oil milling quarter, where thousands of citizens resided on low-lying ground. Hundreds of residential properties were ruined. Infrastructure was also badly affected with the electric light [ing], tramway and telephone services “thrown into disorder”. The railway track at Brough was also left under water (The Times, 1921). Despite much of the reported damage focused on Hull, many other east coast towns were also affected, including Grimsby, Blyth, and Alloa (Met Office, 1921; Hickley 1997; Zong and Tooley 2003; Eden, 2008; Northumberland County Council, 2010). In Dundee, ships were swept into the streets and subsequently moored to lamp posts (The Argus, 1921).


  1. The Argus, 1921. Flood Tide at Hull; Old Town Inundated; Week-end Shoppers Trapped. The Argus. Available at:
  2. Met Office, 1921. Monthly Weather Report of the Meteorological Office. Monthly Weather Report, 43(11). Available at:
  3. Hickey, K.R., 1997. Documentary records of coastal storms in Scotland, 1500-1991 A.D. Coventry University. Available at:
  4. The Times, 1921. Floods at Hull; public buildings and churches damaged. Times Newspapers Limited [London, England]. The Times Digital Archive.
  5. Hickey, K.R., 1997. Documentary records of coastal storms in Scotland, 1500-1991 A.D. Coventry University. Available at:
  6. Zong, Y. & Tooley, M.J., 2003. A Historical Record of Coastal Floods in Britain: Frequencies and Associated Storm Tracks. Natural Hazards, 29(1), pp.13–36. Available at: [Accessed March 5, 2015].
  7. Eden, P., 2008. Great British Weather Disasters, London: Continuum UK.
  8. Northumberland County Council, 2010. Level 1 Strategic Flood Risk Assessment. Apppendix A. Document prepared by Scott Wilson Group plc, Morpeth. Available at: