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Cyclone Namu

South Pacific and Australian region cyclone in 1986

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Severe Tropical Cyclone Namu on May 20, 1986
The National Oceanic and Atmospheric Administration, NCDC · Public domain

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The system impacted the Solomon Islands, Vanuatu and New Caledonia and caused over 100 deaths, as well as varying amounts of damage to the island nations. As a result, the name Namu was later retired from the lists of tropical cyclone names for the South Pacific by the World Meteorological Organization.

The storm's slow motion allowed for prolonged periods of heavy rainfall, resulting in phenomenal flooding across the Solomon Islands. The islands of Malaita and Guadalcanal experienced the most significant damage from Namu. Coastal areas of the former were severely damaged by rough seas and strong winds, especially along the eastern side where entire villages were destroyed. Meanwhile, on the island of Guadalcanal, a village of 43 people had only 5 survivors. Moreover, Cyclone Namu flooded 75% of Guadalcanal's plains. In addition, 22% of homes were either damaged or destroyed on the island.

Across the Solomon Island group, schools, buildings, electricity, water supplies, roads, communication systems, forests, and agriculture sustained widespread damage. In some regions, nearly all homes were destroyed. Mudslides destroyed roads, bridges, water pipes and drainage systems. Crops such as cocoa, copra, coffee, and rice were destroyed. Villages throughout the entire island group sustained severe damage. Overall, approximately 90,000 people, one third of the country's population, were reported as homeless. In all, Cyclone Namu was responsible for at least 150 deaths, mostly from flooding and landslides. Property damage and economic losses across the Solomon Islands totaled $25 million and $100 million (1986 USD) respectively. During the aftermath of the storm, the government of the Solomon Islands declared a national state of emergency. Meanwhile, the United Kingdom, Papua New Guinea, the United States, and Japan also sent supplies and goods to the Solomon Islands.


Meteorological history

On 15 May 1986, the Fiji Meteorological Service (FMS) started to publicly monitor a tropical depression that developed within a monsoon trough to the north of Malaita in the Solomon Islands. The system initially moved eastwards away from the archipelago and showed signs of weakening, as clouds associated with the system dissipated and there were no banding features present. As a result, the FMS was doubtful about the presence of gale-force winds and suspended issuing warnings on the system but continued to monitor it. During 17 May, the system showed signs of reintensifying as it turned and started to move south-westwards back towards the island nation. Later that day, the United States Joint Typhoon Warning Center (JTWC) initiated advisories on it and designated it as Tropical Cyclone 33P, before the FMS reinitiated advisories on the system as it started to rapidly intensify. At around 21:00 UTC (08:00 SIT, 18 May), the FMS determined that the depression had become a tropical cyclone and named it Namu. After being named, Namu intensified as it moved south-westwards towards the Solomon Islands before it passed near or over Manawai Harbour on Malaita at about 14:00 UTC (01:00 SIT, 19 May). The system subsequently changed direction and moved southwards parallel to Malaita's east coast before it crossed the island to the north of Maka.

After crossing Malaita, Namu emerged into the Indispensable Strait, where it was thought to have developed a small ring of marginal hurricane-force winds. According to eyewitness reports obtained after the event, the system made landfall on the island of Guadalcanal near the Marau Sound at about 16:00 UTC (03:00 SIT). Around two hours later, the FMS reported that Namu had peaked with 10-minute sustained winds of 150 km/h (90 mph), which made it a Category 3 severe tropical cyclone on the modern-day Australian scale. While over Guadalcanal, the system appeared to slow down or become near-stationary for three hours as it approached Avuavu before it turned and moved southwards into the Solomon Sea on 19 May. After entering the Solomon Sea, Namu moved out of the South Pacific tropical cyclone basin and into the Australian region, where the Australian Bureau of Meteorology took over the primary warning responsibility from the FMS. The system subsequently passed about 35 km (25 mi) to the northwest of Bellona as it came under the influence of westerly winds that steered it southeastwards. On 20 May, a broad and ragged eye appeared on satellite imagery; however, it quickly became obscured by high clouds. Later that day, the JTWC reported that Namu had peaked with 1-minute sustained wind speeds of 155 km/h (100 mph), which made it a Category 2 hurricane on the Saffir-Simpson hurricane wind scale. During the following day, the system moved back into the South Pacific basin, where it passed to the northeast of Noumea in New Caledonia and rapidly weakened into a depression as it interacted with cooler air. The system was subsequently lost by the FMS during 22 May as it merged with an eastwards-moving trough near southern Vanuatu, before the system was last noted by the JTWC during the following day.

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