Over the next couple of days the system gradually developed further as it moved westwards into the South Pacific basin.

[3][4] The subsequent remnant low continued to move towards the south-southeast before it was last noted by the FMS on February 10, while it was located about 270 km (170 mi) to the east of New Caledonia.

During March 16, a shallow tropical depression developed within the monsoon trough of low pressure about 531 km (330 mi) to the northwest of Nadi, Fiji.

The system subsequently peaked with 10-minute sustained winds of 45 knots during the next day, before it started to accelerate south-eastwards and rapidly weaken.

The system was last noted during March 21, while it was located about Cyril caused significant flooding within Fiji's Northern and Western divisions, with a peak of 5.62 m (18.4 ft) reported during March 18 within the town of Nadi, while a small storm surge of 0.3 m (0.98 ft) was observed within Nadi's bay on the same day.