by RSMC Nadi on January 24. During January 22, RSMC Nadi also started monitoring Tropical Disturbance 10F, which had developed around to the northeast of Port Vila, Vanuatu. The system lied within an area of moderate to high vertical windshear to the north of an upper-level ridge of high pressure. Over the next couple of days the system moved westwards into an area of low vertical windshear and the Australian region, where it developed into Tropical Cyclone Dylan during January 26. Tropical Disturbance 11F subsequently developed to the southwest of Nadi, Fiji during January 29. The system lay to the east of an upper-level trough of low pressure within an area of high vertical windshear. During that day the system moved towards the east-southeast and was subsequently last noted by RSMC Nadi later that day as it moved into TCWC Wellingtons area of responsibility. During February 23, RSMC Nadi reported that Tropical Disturbance 14F had developed, within a trough of low pressure to the north-northwest of Maewo, Vanuatu. Over the next day the system moved slowly towards the south-southeast and developed into a tropical depression. Over the next two days the system continued to move towards the south-southeast and prompted heavy rain warnings for Fiji, before it dissipated during February 26. Late on February 26, RSMC Nadi reported that Tropical Disturbance 16F, had developed about south of the Indispensable Reefs. Over the next day the system moved westwards and moved into the Australian region, where it eventually developed into Tropical Cyclone Hadi during March 9. On March 6, RSMC Nadi reported that Tropical Disturbance 17F had developed about to the northeast of Port Vila, Vanuatu. Over the next two days the system remained weak as it moved south-westwards, before it was last noted during March 8, as it moved into an area of moderate to high vertical windshear and the Australian Region. Tropical Cyclone Hadi subsequently moved back into the South Pacific basin late on March 12, where RSMC Nadi designated it as Tropical Disturbance 20F. On March 18, the Tropical Disturbance re-exited the South Pacific basin into the Australian basin. The last tropical disturbance of the season: 21F, formed on March 17, about to the north of Rarotonga in the Cook Islands, before dissipating two days later. Season effects This table lists all the storms that developed in the South Pacific to the east of longitude 160°E during the