Cyclone Yali
Severe Tropical Cyclone Yali was one of seven severe tropical cyclones to develop during the 1997–98 South Pacific cyclone season. The system that was to become Yali was first noted as a tropical disturbance, to the northeast of Vanuatu during 17 March. Over the next couple of days, the system moved towards the south-west and gradually developed further, before it was named Yali during 19 March, after it had developed into a tropical cyclone. After it was named Yali re-curved and started moving towards the south-southeast, as the monsoonal flow to the north of the system strengthened. While the system was active, Yali affected Vanuatu and New Caledonia before the extra-tropical remnants impacted New Zealand where a man was killed and widespread power outages and damage were reported.
Meteorological history
During 17 March, the United States Joint Typhoon Warning Center issued a tropical cyclone formation alert on a tropical disturbance, that had developed about to the northeast of Port Vila in Vanuatu. The disturbance was slowly moving south-southwestwards, along the steering flow of a weak mid-level ridge of high pressure in between Vanuatu and the Solomon Islands. Over the following day, the Fiji Meteorological Service started to monitor the disturbance, as a well defined area of low pressure, while the JTWC subsequently initiated advisories and designated the system as Tropical Cyclone 29P. During 19 March, the system continued to develop in an area of low vertical wind shear and warm sea surface temperatures, before the FMS named it Yali after it had developed into a Category 1 tropical cyclone on the Australian tropical cyclone intensity scale. The newly named tropical cyclone subsequently started to move south-eastwards, as the monsoonal steering flow to the north of the system increased.After passing west of Vanuatu, this storm gradually intensified; by 21 March, the JTWC reported that Yali had intensified into a Category 1 hurricane.
During 22 March, the JTWC reported that Yali had peaked with 1-minute sustained wind speeds of, which made it equivalent to a category 2 hurricane on the Saffir-Simpson hurricane wind scale. Later that day, the FMS followed suit and reported that Yali had peaked with 10-minute sustained wind speeds of, which made it a Category 3 severe tropical cyclone.
During that day Yali passed about to the west of the capital city of Vanuatu: Port Villa, before passing over the Vanuatuan islands of Tanna and Aneityum.
Shortly after its peak, thunderstorm activity began to decrease, and Yali started weakening. On 22 March, the JTWC noted that winds had subsided to tropical storm status while winds soon dropped below Category 2 intensity. At around the same time, a mid-level subtropical ridge began to influence its motion, sending it to the west. As Yali moved to the southwest, the wind field became asymmetric. Based on Nadi data, by 23 March, Yali was just east of Nouméa, New Caledonia with winds of 50 mph. After passing south of New Caledonia, an upper-level low picked up the cyclone and induced cold air into the atmospheric circulation.
Early on 25 March, Yali had lost its tropical characteristics as an upper-level low captured the system, with cold air working around the northern and western sides of the circulation. However, the JTWC continued to monitor Yali as a tropical cyclone, while the system moved across 160°E and into the Australian region, where they were monitored by the Australian Bureau of Meteorology as an extratropical cyclone.
By the next day, Yali's center was less than east-northeast of Brisbane, Australia. Despite a brief revival of convection, on the morning of 27 March, the JTWC released its final bulletin on Yali. At this time, the low was located around east-southeast of Brisbane. The remnants of Yali went under a transformation in the Tasman Sea and respectively deepened south of New Zealand.
The extratropical remnants of Yali were last noted by TCWC Wellington during 31 March, while they were located about to the southeast of Wellington, New Zealand. The remnants were subsequently absorbed into the circumpolar trough.