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North Sea flood of 1953

North Sea flood of 1953 is a science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand North Sea flood of 1953 rather than just read about it. In short: The North Sea flood of 1953, also known as the Big Flood or East Coast Flood (in England) or as the Flood Disaster (Dutch: Watersnoodramp), was a flood caused by a heavy storm surge in the North Sea that struck low-lying coastal areas of the Netherlands, Belgium, and the United Kingdom. More than 2,000 people were killed on land and hundreds more at sea.

North Sea flood of 1953 — main illustration
North Sea flood of 1953 — illustration

Key takeaways

  • North Sea flood of 1953 belongs to science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect North Sea flood of 1953 to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of North Sea flood of 1953 from memory before moving on to harder problems.

Reference excerpt

The North Sea flood of 1953, also known as the Big Flood or East Coast Flood (in England) or as the Flood Disaster (Dutch: Watersnoodramp), was a flood caused by a heavy storm surge in the North Sea that struck low-lying coastal areas of the Netherlands, Belgium, and the United Kingdom. More than 2,000 people were killed on land and hundreds more at sea. It was the worst natural disaster of the 20th century in the United Kingdom and the worst in the Netherlands since the Middle Ages. The storm and flooding occurred during the night of Saturday, 31 January to the morning of 1 February 1953. A combination of a high spring tide and a severe European windstorm caused a storm tide of the North Sea. Most sea defences facing the surge were overwhelmed, resulting in extensive flooding. The combination of wind, high tide, and low pressure caused the sea to flood land up to 5.6 metres (18 ft 4 in) above mean sea level. Realising that such infrequent events could reoccur, the Netherlands and the United Kingdom carried out large studies on strengthening of coastal defences. The Netherlands developed the Delta Works, an extensive system of dams and storm surge barriers. The UK constructed storm surge barriers on the Thames Estuary and on the Hull where it meets the Humber Estuary.

Flooding summary At the time of the flood, 20% of the land of the Netherlands was below mean sea level (subsequently, with the expansion of Flevoland, this proportion has increased), and the next-highest 30% sat at less than 1 metre (3.3 ft) above sea level. Such land relies heavily on sea defences and was worst affected, recording 1,836 deaths and widespread damage. Most of the casualties occurred in the province of Zeeland. In England, 307 people were killed in the counties of Lincolnshire, Norfolk, Suffolk and Essex. Nineteen were killed in Eastern Scotland. Twenty-eight people were killed in the north of West Flanders, Belgium.

Fatalities at sea More than 230 deaths occurred on seacraft along Northern European coasts as well as on ships in deeper waters of the North Sea. The Stranraer–Larne car ferry MV Princess Victoria sank in the North Channel east of Larne with 134 fatalities, and many fishing trawlers sank. Nine small vessels foundered in the seas around the British Isles with the loss of all hands; these included the Swedish steamer Aspo (22 crew lost), the British steamer Yewvalley (12 crew lost), the British trawlers Sheldon (14 crew lost), Michael Griffith (13 crew lost) and Guava (eleven crew lost), the Dutch motor vessels Salland (nine crew lost) and Westland (eight crew lost), the Dutch trawler Catharina Duyvis (16 crew lost), and the Belgian trawler Leopold Nera (five crew lost).

Netherlands

From midday on 31 January 1953, water was driven from the northern reaches of the North Sea between Norway and Scotland by a strong northwest gale. A storm surge developed along the coast of the Netherlands, which coincided with a high spring tide, leading to many water levels on the Dutch coast on the morning of 1 February 1953 being higher than any previous recorded figures, particularly in the southwestern areas of the country. At 10:30 p.m. on Saturday evening 31 January, it was low tide but, this time, the water remained high. The strength of the hurricane had broken the tidal movement. On the night of 1 February 1953 around 3 a.m., many dykes in the province of Zeeland and adjacent areas of South Holland and North Brabant proved unable to resist the floodwaters. On both islands and mainland, large areas of the country were flooded. At 4 p.m. on 1 February, the flood reached a second high. The water rose even higher than during the first flood, and more dykes broke. Many people who had survived the first flood died, as the houses whose rooftops they had sheltered on collapsed due to the persistent water pressure. At that time, the government did not yet know that Schouwen-Duiveland, Goeree-Overflakkee and Tholen were almost completely under water, and no large-scale rescue operations had yet taken place. Only on Monday 2 February were fishermen the first to sail deep into the disaster area to save hundreds of people. Rescue operations from the air were hardly possible: the Netherlands had only 1 helicopter and had to wait until other countries offered help. On Tuesday 3 February, a large flow of people and relief supplies started. Planes dropped sandbags, dinghies, boots, food and water over the disaster area. At the same time, thousands of Dutch soldiers, administrators, aid workers and volunteers arrived to carry out coordinated actions in the disaster area. Tens of thousands of residents were being evacuated from the area to shelters elsewhere in the country. Foreign helicopters and amphibious vehicles also came into action on Tuesday, but the vast majority of rescue operations had already been completed by then. Donations and relief supplies were pouring in at the National Disaster Fund in The Hague. Other countries, including Britain, Sweden and Canada, sent more than 61 million guilders in relief supplies. Many people still commemorate the dead during the Herdenking Watersnoodramp on 1 February.

Warnings Rijkswaterstaat had warned about the risk of a flood. At the time of the flood, none of the local radio stations broadcast at night, and many of the smaller weather stations also only operated during the day. The following broadcast from the Royal Netherlands Meteorological Institute (KNMI) was made at 6.15pm (18:15) on 31 January 1953 on Hilversum Radio:

… excerpt ends here. Continue reading the full article.

Illustrations

North Sea flood of 1953 illustration
North Sea flood of 1953: Synoptic chart at midnight 1 February 1953
Synoptic chart at midnight 1 February 1953
North Sea flood of 1953: Extent of flooding in the Netherlands
Extent of flooding in the Netherlands
North Sea flood of 1953: Een dubbeltje op zijn kant ("A dubbeltje on its edge", meaning 'a narrow escape'), a sculpture by Roel Bendijk of de Twee Gebroeders in the Groenedijk. 

'Dubbeltje' (lit. 'little double') was a thin, former Dutch coin
Een dubbeltje op zijn kant ("A dubbeltje on its edge", meaning 'a narrow escape'), a sculpture by Roel Bendijk of de Twee Gebroeders in the Groenedijk. 'Dubbeltje' (lit. 'little double') was a thin, former Dutch coin
North Sea flood of 1953: A breach at Erith after the 1953 flood
A breach at Erith after the 1953 flood

Worked examples

Example 1 — a first encounter with North Sea flood of 1953

Start with the simplest possible case. Write down what North Sea flood of 1953 claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to North Sea flood of 1953 before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about North Sea flood of 1953 ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of North Sea flood of 1953

In research
North Sea flood of 1953 appears in science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses North Sea flood of 1953 in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
North Sea flood of 1953 is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1950s floods in Europe, 1953 disasters in Belgium, 1953 disasters in Europe, so understanding it makes those chapters shorter.
In everyday life
Look for North Sea flood of 1953 outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study North Sea flood of 1953 in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what North Sea flood of 1953 means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain North Sea flood of 1953 out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is North Sea flood of 1953 in simple terms?

The North Sea flood of 1953, also known as the Big Flood or East Coast Flood (in England) or as the Flood Disaster (Dutch: Watersnoodramp), was a flood caused by a heavy storm surge in the North Sea that struck low-lying coastal areas of the Netherlands, Belgium, and the United Kingdom. More than 2…

Why does North Sea flood of 1953 matter?

Because it connects several science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study North Sea flood of 1953?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on North Sea flood of 1953.

Tags

  • 1950s floods in Europe
  • 1953 disasters in Belgium
  • 1953 disasters in Europe
  • 1953 disasters in the Netherlands
  • 1953 disasters in the United Kingdom
  • 1953 in Belgium
  • 1953 in England
  • 1953 in Scotland
  • 1953 in radio
  • 1953 in the Netherlands
  • 1953 natural disasters
  • Amateur radio emergency communications

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