system, before it was during October 20 as it dissipated to the north of Vanuatu. During the following day Tropical Disturbance 03F developed within an area of low shear, about to the northeast of Honiara on Guadalcanal in the Solomon Islands. The system was last noted during October 22, after convection surrounding the centre had significantly reduced. On October 25, the FMS reported that Tropical Depression 04F had developed under an upper-level ridge of high pressure within an area of low windshear, about to the southeast of Honiara. Over the next couple of days the system affected the Solomon Islands, before it was last noted during October 27, as it was not expected to develop into a Category 1 tropical cyclone. A reanalysis of these three systems was performed by Steve Young during April 2014, who felt that these three systems represented one weak system that existed between October 18–27, near the Solomon Islands. On December 9, RSMC Nadi reported that Tropical Disturbance 05F had developed to the east of an upper-level trough, in an area of moderate to high vertical windshear about to the northeast of Nadi, Fiji. During that day the system moved towards the southeast and passed over the Fijian island of Viti Levu. After passing over Fiji the system continued to move south-eastwards and developed into a tropical depression during December 11. During December 12, the system passed about to the south of Tongatapu Island, before RSMC Nadi issued its final advisory on the system during the next day, as the system was not expected to develop into a tropical cyclone. On December 23, RSMC Nadi reported that Tropical Disturbance 06F had developed under an upper-level ridge of high pressure, within an area of moderate vertical wind shear to the northeast of the Santa Cruz Islands. Over the next few days the system moved south-eastwards and influenced the "moist easterly wind flow" over the Fijian Islands until it was last noted during December 29. Late on January 21, RSMC Nadi reported that Tropical Depression 09F had developed about to the southwest of the Cook Island: Palmerston. Over the next day the system moved westwards and developed into a tropical depression, while located within an area of low to moderate vertical windshear. Over the next couple of days the JTWC also monitored the system as a subtropical system that was becoming tropical, before it was last noted