[8] As a tropical cyclone, Yasi brought significant rain to both Fiji and Tonga before it dissipated on January 19 to the south of Papette in French Polynesia.

[11] On March 9 and 10, Tropical Cyclones Zaka and Atu both developed near New Caledonia, about 1,000 km (620 mi) apart and took similar tracks towards the southeast before becoming extratropical.

[2] On January 12, the FMS reported that a tropical depression had developed over the Fijian island of Vanua Levu, about 430 km (270 mi) to the south of Labasa.

[12] During the following day, the depression rapidly developed further as it interacted with the South Pacific Convergence Zone, before the NPMOC initiated warnings on the system and designated it as 08P.

[8][13] On March 9, the FMS started to monitor a tropical depression had developed within an active convergence zone, about 150 km (93 mi) to the northwest of Nouméa, New Caledonia.

[3] The FMS then issued their final advisory at 0600 UTC, as Zaka had weakened into a tropical depression and was moving into TCWC Wellingtons area of responsibility.

[16] On March 4, the JTWC started to monitor an area of disturbed weather that had developed within the Australian region about 900 km (560 mi), to the southeast of Port Moresby in Papua New Guinea.

[8] During that day, Beti continued to develop further before the system moved into the Coral Sea on March 24, after passing over the Vanuatuan islands of Pentecost and Malekula.

[8] Later on March 28, the FMS passed the primary warning responsibility of the cyclone to MetService, before the JTWC issued their final advisory on Beti as it had become extratropical.

[8] The most significant damage occurred in New Caledonia where wind and flooding destroyed crops, gardens and caused disruption to the electricity network, water supply, road and telephone communications.

[nb 2][22][23] As an extratropical cyclone, Beti generated a high surf and long period swells that hit both eastern Australia and New Zealand.

[8] During December 23, the remnants of Severe Tropical Cyclone Gertie, moved westwards off the Australian mainland and into the Coral Sea near Maryborough.

[10] After moving into the Coral Sea, the system underwent a pierod of rapid intensification, during which it reintensified into a tropical cyclone and caused gale-force winds along the southern Queensland Coast.

[10][25] During the following day, gale-force winds eased along the Queensland coast, as Gertie moved north-eastwards into the South Pacific basin, where it peaked with 10-minute sustained windspeeds of 75 km/h (45 mph).

[8] Over the next 24 hours the low deepened to about 1002 hPa (29.59 inHg) before it crossed 160°E and moved into the Australian region where it became known as the Queen Elizabeth II storm.

[8] On February 22 and 23, a shallow tropical depression moved around the Fijian archipelago and caused some flooding of low-lying areas in Vanua Levu.