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Cyclone Dovi (2022)

South Pacific tropical cyclone

  • 8 min read
  • 3 chapters

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Through World Bank Group and Landslide

Meteorological history

On February 4, the United States Joint Typhoon Warning Center reported that a tropical disturbance, had developed within the Australian region about 1,285 km (800 mi) to the west of New Caledonia. The disturbance was starting to develop a low-level circulation, which was accompanied by fragmented atmospheric convection, along a frontal boundary that extended across the Cape York Peninsula and the Coral Sea. Over the next couple of days, the Australian Bureau of Meteorology (BoM) and the Fiji Meteorological Service (FMS) started to monitor the poorly organized system as Tropical Low 18U and Tropical Disturbance 08F, as it moved eastwards within the frontal boundary towards Vanuatu and the South Pacific basin. During February 7, the system started to slowly consolidate, as it passed to the north of New Caledonia, before the FMS classified the system as a tropical depression. At this stage, the depression was moving eastwards and was predicted to continue to move eastwards towards Fiji, however, the depression slowed down as it approached the islands of southern Vanuatu during February 8.

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