Rewa was the longest-lived South Pacific tropical cyclone on record, lasting 25 days, from 26 December to 21 January.

The ridge built behind the trough, causing the depression to stall and drift northward, and by 22 February, Farah dissipated.

[6] During 29 January, the BoM reported that a tropical low had developed within the monsoon trough, to the north of the Gove Peninsula in the Northern Territory.

[7][9][10] Early the next day Cyclone Sadie made landfall to the north of near Normanton, after the BoM had reported that the system had peaked with 10-minute maximum sustained winds of 85 km/h (50 mph).

It formed about 1100 km north of Northwest Cape on 12 March 1994, then rapidly intensified during the 14th while moving on a south-southwest path towards the west Pilbara coast.

[6] Tropical Cyclone Tim was a very small weak system that moved on a generally westward path from south of Sumatra to the Cocos Islands from 28 March to 3 April 1994.

Its development from here on was hampered by vertical wind shear and Vivienne moved on a generally west-southwest path parallel to, but well offshore from, the Western Australian coastline.

[6] On 20 April, the JTWC started to monitor an area of low pressure that located over the Solomon Islands about 155 km (95 mi) to the north of Honiara.

[11][12] As a result of the windshear, the center became exposed and displaced from the deep convection before the JTWC issued their final advisory on 25 April as 29P weakened into an area of low pressure, before dissipating later that day about 600 km (375 mi) to the southwest of Honiara.

[7][13] Over the next day the system moved eastwards and gradually developed further, before TCWC Port Moresby reported that the system had developed into a category 1 tropical cyclone on the Australian scale and named it Usha during the next day before it moved into the South Pacific tropical cyclone basin.