Libya flooding of 2023

print Print
Please select which sections you would like to print:
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Feedback
Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login).
Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

External Websites
Quick Facts
Date:
September 10, 2023 - September 11, 2023
Location:
Libya

Libya flooding of 2023, catastrophic flooding that struck eastern Libya on September 10 and 11, 2023. More than 4,000 people were killed and some 10,000 were missing after heavy rains generated by Storm Daniel (a strong Mediterranean cyclone) drenched the area and brought flooding to the region. About 25 percent of the Libyan port city of Derna was destroyed by a massive torrent of water and mud after two dams located upstream from the city collapsed from pressure brought on by the heavy rains. Roughly one week earlier, flash flooding caused by Daniel had damaged infrastructure and inundated villages in Greece, Bulgaria, and western Turkey.

Storm Daniel’s heavy rains

The weather system that brought unusually heavy rains to eastern and central Mediterranean was Storm Daniel, a strong mid-latitude cyclone that developed over the Ionian Sea and Greece in early September (see also climate: Cyclones and anticyclones). Daniel’s resemblance to a tropical storm in both shape and intensity prompted some meteorologists to refer to Daniel as a “medicane” (a portmanteau of Mediterranean hurricane). Daniel was held in place by a blocking high-pressure system over the Netherlands, whose movement was restricted by another low-pressure system to its west, which created a weather phenomena called an omega block (a configuration that resembles the Greek letter omega, Ω, on weather maps).

Fueled also by unusually warm sea-surface temperatures in the Mediterranean Sea, Daniel strengthened rapidly, delivering torrential rains and high winds to the southern Balkan peninsula and western Turkey starting on September 4. Parts of central Greece received as many as 29.5 inches (750 mm) of rain—almost the same amount the area typically receives in one year—in only 24 hours. Daniel also generated waterspouts (small-diameter columns of rapidly swirling air in contact with a water surface) in the Aegean and Tyrrhenian seas. The storm then tracked southwest over the Ionian Sea before bending southeast toward eastern Libya.

Daniel’s high winds and heavy rains peaked over eastern Libya during the morning of September 10. Bolstered by warm waters measuring 27.5 °C (81.5 °F) off the Libyan coast, Daniel generated tropical-storm-force winds ranging from 43.4 to 49.6 miles (70 to 80 km) per hour, which downed trees and electrical towers, and drenched coastal cities, producing flash floods. Across much of the region, cities and towns measured between 5.9 and 9.4 inches (150 and 240 mm) of rainfall; however, the highest 24-hour rainfall total, 16.3 inches (414 mm), occurred in Zāwiyat al-Bayḍāʾ, which is roughly 5 miles (8 km) from the coast in the Akhḍar Mountains.

Damage

Daniel’s winds and rain produced extensive damage across the southern Balkan Peninsula, western Turkey, and eastern Libya. The Libyan coastal city of Derna and its population of more than 100,000 inhabitants, however, were hardest hit by the effects of the storm. Whereas rising waters claimed the lives of 4 people in Bulgaria, 7 people in Turkey, 17 people in Greece, and about 170 people in other cities in eastern Libya, thousands were killed in Derna after the Abu Mansour and Derna (Belad) dams, which had suffered from years of neglect, failed. The collapse of the dams sent nearly 7.9 billion gallons (30 million cubic meters) of water downstream along the Wadi Derna river, which bisects the city. A wave of reddish mud measuring about 23 feet (7 meters) high struck in the middle of the night—crushing houses, washing out the lower floors of high-rises, and sending people, vehicles, and debris into the sea. By some estimates, the deluge destroyed or heavily damaged at least one-quarter of the city, leaving about 400 structures submerged in thick mud.

In the days after the disaster, the Libyan Red Crescent reported that 11,300 people had been killed and 10,100 people were missing in Derna alone. On September 20, however, the UN Office for the Coordination of Humanitarian Affairs, citing World Health Organization estimates, revised its figures downward to 3,958 dead and 9,000 missing in Libya.

In Greece, Turkey, and Bulgaria, floodwaters also immersed villages and infrastructure. Damage was most pronounced in Greece’s Thessaly region, where some 280 square miles (720 square km) were flooded, with news reports noting that some villages were covered by 9.8 feet (3 meters) of water. The floods also cut or damaged roads, buildings, train lines, and other infrastructure within and near the cities of Larissa and Volos while also spreading a thick layer of flood-driven silt across croplands, effectively halting the year’s harvest of cotton, tobacco, and other crops and threatening future yields.

Get Unlimited Access
Try Britannica Premium for free and discover more.

Relief and recovery

Rescue efforts began in both of the affected regions almost immediately after Daniel’s passage. In Greece, civil authorities rescued some 1,700 people, with nearly 300 being taken to safety by helicopter. While no specific damage estimates were available following the storm, Greek government officials estimated that Greece’s recovery from the storm alone could cost billions of euros, whereas regional experts examining the financial impact of the storm across the Mediterranean expected that Daniel would become the costliest Mediterranean storm on record.

In eastern Libya, the flooding forced an estimated 40,000 people out of their homes, with some 30,000 being displaced in Derna alone. While many in damaged areas outside Derna were able to relocate to other cities, Daniel wreaked havoc on Derna’s road and bridge infrastructure—which, when combined with the country’s poorly run governmental bureaucracy—hampered the movement of refugees, rescue crews, government services, and aid. The first emergency deliveries were much delayed, arriving some 36 hours after the onset of the disaster. In the days after, additional aid and staffing arrived by plane, with the International Federation of Red Cross and Red Crescent Societies (IFRC) and other organizations assisting the Libyan government with relief and recovery; however, the pace of their collective efforts was not keeping up with the needs of residents. UN relief officials and others noted that the city was facing shortages of medicine, food, and shelter and were concerned that rising mud-contaminated water could sicken survivors in the coming weeks and months.

More than a week after the disaster, Derna remained a city in disarray, as relief groups continued to recover and bury bodies that had washed up on the shores and had been covered by the mud. By September 18, frustrated Derna residents had gathered to protest the slow government response, and Libyan government officials and troops deployed to Derna had begun to divide the city into sections, a measure put in place ostensibly to slow the spread of potential disease outbreaks. By September 19, Libyan government officials had reported that more than 3,300 bodies had been recovered and buried, many in mass graves.

The role of climatic change

A number of meteorologists and climate scientists noted that climate change very likely played a significant role in increasing Daniel’s intensity. A study by the World Weather Attribution group in the days that followed examined factors affecting the storm and determined that such a rainfall event occurring in eastern Libya would be expected to happen only once every 300 to 600 years. It suggested that factors related to climate change, such as the global average temperature being 1.2 °C (2.2 °F) warmer than that of pre-industrial times (that is, before 1750), made the Libyan rainfall event 50 percent more intense and 50 times more likely to occur and the rainfall events in Greece, Bulgaria, and Turkey 40 percent more intense and 10 times more likely to occur.

John P. Rafferty