2018–19 South Pacific cyclone season

Category 1 tropical cyclone (Australian scale)
Tropical storm (SSHWS)
Duration	September 26 (Entered basin) – September 28 (Exited basin)
Peak intensity	75 km/h (45 mph) (10-min); 994 hPa (mbar)

A disturbance which initially formed in the Australian region basin crossed into the South Pacific basin on September 26 and strengthened, and was designated as Tropical Depression 01F by RSMC Nadi.[5] Late on September 26, the storm intensified into a tropical cyclone, and was given the name Liua. Liua is the earliest-forming named tropical cyclone in the South Pacific basin since reliable records began, surpassing Cyclone Lusi in 1997.[6]

Tropical disturbance (Australian scale)
Duration	November 11 – November 16
Peak intensity	Winds not specified; 1003 hPa (mbar)

During November 11, the FMS reported that Tropical Disturbance 02F had developed about 340 km (210 mi) to the north-northeast of Honiara in the Solomon Islands.[7] At this stage the system was located within an area of low vertical windshear, while deep convection surrounding the system's low level circulation was poorly organised. Over the next few days, the system's organization slightly improved as it moved south-eastwards, before it was last noted during November 16, while located about 575 km (355 mi) to the northeast of Port Vila in Vanuatu.

Tropical depression (Australian scale)
Duration	December 28 – January 1
Peak intensity	55 km/h (35 mph) (10-min); 998 hPa (mbar)

During December 28, the FMS reported that Tropical Disturbance 03F had developed within a trough of low pressure, about 685 km (425 mi) to the east of Honiara in the Solomon Islands.[8] The disturbance was located within a favourable environment for further development to the south of an upper-level ridge, while deep atmospheric convection persisted over the systems elongated low-level circulation.[8][9] During the next day, as the organisation of the system improved, the FMS relocated the system to be located near the Solomon Island of San Cristobal.[10] The system subsequently moved eastwards through Temotu Province and gradually developed further, before it was classified as a tropical depression during December 30. It dissipated on January 1.

Category 2 tropical cyclone (Australian scale)
Tropical storm (SSHWS)
Duration	December 31 (Entered basin) – January 7
Peak intensity	95 km/h (60 mph) (10-min); 985 hPa (mbar)

Mona entered this basin as a tropical low from the Australian region basin. The system then intensified into Tropical Depression 04F on January 3. Later that day, it intensified into a Category 1 cyclone on the Australian scale and was named Mona. It peaked as a Category 2 tropical cyclone. On January 7, the system dissipated.

About 2,000 people took shelter in 40 evacuation centers over the weekend, and thirty roads were closed, mostly due to floods and some landslides. People in the Lau group have been warned to expect gale-force and heavy rain as Mona tracked south, before arching south-west over Fiji over the next 24 hours.[11]

Tropical disturbance (Australian scale)
Duration	December 31 – January 2
Peak intensity	Winds not specified; 998 hPa (mbar)

On December 31, the FMS noted that Tropical Disturbance 05F formed. The disturbance peaked at 998 mbar. After its peak intensity, the disturbance started a weakening trend that continued until January 2, where the disturbance had dissipated completely.

Tropical depression (Australian scale)
Duration	February 3 – February 9
Peak intensity	Winds not specified; 994 hPa (mbar)

On February 3, Tropical Depression 06F formed to the north of Fiji. The system moved in a south-easterly direction and was predicted to reach Category 1 status while the system was located to the NNW of Niua Fo'ou Island. However, due to strong wind shear and cool air flowing from the south of the system, 06F was not named. Tonga was largely affected by TD 06F. On the island, gale-force winds flattened banana plantations and crops, especially the casava plant. The system disrupted schools and transportation. All schools were cancelled on Friday, February 8 and all sea and air transportation was disrupted. It dissipated on February 9.

On Saturday, the Cyclone Alert and Gale warning that was issued for Tonga regarding TD 06F was lifted. However, another Tropical Cyclone Formation Alert was issued together with new warnings was issued regarding the thread from TD 07F (which later become Neil) which recently formed north of Fiji. TD 06F was one of 4 tropical systems to directly impact the island nation (the others are Tropical Cyclone Neil, Tropical Depression 08F and Tropical Depression 10F) within 1 week.

Category 1 tropical cyclone (Australian scale)
Tropical storm (SSHWS)
Duration	February 8 – February 10
Peak intensity	65 km/h (40 mph) (10-min); 994 hPa (mbar)

On February 8, a tropical low developed into Tropical Depression 07F. The system intensified into a Category 1 tropical cyclone on February 9, 2019, and was assigned the name Neil. The system reached its peak intensity later that day with 10-minute sustained winds of 65 km/h (40 mph). On February 10, Neil weakened into a tropical depression, before dissipating soon afterward. Tonga issued warnings for Neil while it was active, but lifted those warnings once the storm weakened. No structural damage was reported from the storm.[12]

Category 3 severe tropical cyclone (Australian scale)
Category 1 tropical cyclone (SSHWS)
Duration	February 11 (Entered basin) – February 22
Peak intensity	130 km/h (80 mph) (10-min); 974 hPa (mbar)

On February 7, a tropical low developed within an active monsoon trough, along the coast of Vanuatu.[13]

The low crossed into the South Pacific Basin and began intensifying into a tropical cyclone on February 11, earning the name Oma, and quickly reaching Category 2 tropical cyclone intensity.

It then strengthened into a severe tropical cyclone on February 15, reaching its initial peak intensity on February 16, as a Category 3 tropical cyclone on the Australian region scale. Oma then briefly weakened on February 17, before it restrengthened into a severe tropical cyclone and reached its peak intensity on February 19. Oma exited the South Pacific basin and returned to the Australian Region as a tropical cyclone on February 21. Oma weakened to a Category 2 tropical cyclone while approaching the Australian coast. On February 22, Tropical Cyclone Oma crossed over into the South Pacific basin once again. Late on February 22, Oma transitioned into an subtropical cyclone, while turning to the northeast. For the next several days, Oma continued drifting northeastward, weakening further into a subtropical depression on February 25. On February 27, Oma turned eastward, while situated over Vanuatu, and the storm subsequently dissipated on February 28.

Persistent heavy rain, damaging surf, and strong winds battered the northern provinces of Malampa, Sanma, Torba in Vanuatu for several days. Storm surge inundated coastal communities on February 17, extending up to 50 m (160 ft) inland in some areas. Multiple traditionally constructed homes were destroyed while flooding from swollen rivers washed out roads. The strong winds downed trees across the affected region. Communications with Torba were disrupted, with authorities unable to reach the Torres Islands.[14]

Damaging winds up to 140 km/h (87 mph) and heavy rain from the cyclone had battered New Caledonia, leaving thousands of residents without power and isolating some villages.[15] Agriculture was particularly hard-hit with losses reported in all provinces. The French government declared a state of calamity, directed at agriculture, for the entire island which freed ₣150 million (US$1.43 million) for recovery.[16]

Oma sunk a bulk carrier near the Solomon Islands, and it resulted in an oil spill. The cleaning cost were about US$50 million.[17]

Category 4 severe tropical cyclone (Australian scale)
Category 3 tropical cyclone (SSHWS)
Duration	February 23 – March 2
Peak intensity	165 km/h (105 mph) (10-min); 950 hPa (mbar)

During February 23, the FMS reported that Tropical Disturbance 11F had developed, about 525 km (325 mi) to the northwest of Apia, Samoa. The system gradually organized while slowly moving southward. Situated in an environment with sea surface temperatures of 28-30 degrees Celsius and low vertical wind shear, the system intensified into Tropical Cyclone Pola on February 26. Later that day, Pola intensified into a Category 2 tropical cyclone, before becoming a severe tropical cyclone on February 27. On February 28, the system reached its peak intensity, as a Category 4 tropical cyclone on the Australian scale, with 10-minute sustained winds of 105 mph (170 km/h) and a minimum central pressure of 950 hPa (mbar). On March 1, Pola began to weaken while turning eastward, as a result of cooler sea surface temperatures and shear from a high-pressure system over New Zealand. Early on March 2, Pola weakened into a subtropical depression, before dissipating later that day.

Tropical depression (Australian scale)
Duration	May 16 – May 21
Peak intensity	55 km/h (35 mph) (10-min); 1002 hPa (mbar)

On May 16, the FMS started tracking a disturbance for possible cyclone development north of Fiji, in an environment of moderate wind shear and sea surface temperatures of 30 °C (86 °F). By May 18, the FMS classed the system as a tropical depression, giving it the identifier 12F, and they forecast the system to reach tropical cyclone intensity within 12–24 hours, and to ultimately attain 10-minute sustained winds of 85 km/h (55 mph). Later the same day, 12F began to move towards the southeast, and the FMS reported that the system was unlikely to intensify further, due to moderately-high wind shear in the area.

On May 7, the Bureau of Meteorology (BOM) reported that a weak tropical low had developed within a low-pressure trough, to the east of the Solomon Islands.[18] Over the next couple of days, the system gradually moved south-westwards and moved into the Australian region during May 10, where it later developed into a Category 2 tropical cyclone, and received the name Ann from the BOM.