Cyclone Amos
Severe Tropical Cyclone Amos was a strong tropical cyclone that affected the Fijian and Samoan Islands as well as Wallis and Futuna. Amos was first noted as Tropical Disturbance 17F during April 13, 2016 to the northwest of Fiji. The system subsequently moved south-eastwards towards the Fijian Islands, before it passed near or over Vanua Levu during April 16. After passing over Fiji, the system gradually developed further as it moved north-eastwards towards the Samoan Islands. The system was subsequently named Amos during April 20, after it had developed into a tropical cyclone and started to move north-westwards towards the island nation of Tuvalu.
Meteorological history
Tropical Disturbance 17F was first noted by the Fiji Meteorological Service on April 13, while it was located about to the northwest of the Fijian dependency of Rotuma. The system was located underneath an upper level anticyclonic circulation and within an area of low vertical wind shear. Over the next couple of days the system moved westwards, before it started moving south-eastwards towards Fiji during April 15. The system was subsequently classified as a tropical depression on April 16, as passed near or over several islands in Fiji's Northern Division including Vanua Levu. Over the next couple of days 17F moved north-eastwards towards the Samoan Islands and passed about to the west of Tonga's Niuas island group during April 18. A tropical cyclone formation alert on the system was issued by the United States Joint Typhoon Warning Center during that day, as the well defined low level circulation centre consolidated. The depression subsequently started to move north-westwards towards the island nation of Tuvalu, under the influence of a subtropical ridge of high pressure. The system subsequently passed in between the islands of Wallis and Futuna, as a tropical depression during April 19.Early on April 20, the JTWC initiated advisories on the system and designated it as Tropical Cyclone 20P, while the system was located about to the west of Avata, Samoa. Later that day, the FMS named the depression Amos, after the system had developed into a Category 1 tropical cyclone on the Australian tropical cyclone intensity scale. However, further development of the system at this time was restricted by a trough of low pressure to the northeast of the system, which was causing subsidence over the systems north-eastern quadrant. Amos subsequently slowed down later that day and became nearly stationary, as a near-equatorial ridge of high pressure became the primary steering mechanism. As a result of this new primary steering mechanism, the system turned eastwards and moved towards the Samoan Islands. As the system moved eastwards it started to rapidly intensify further, with an eye feature developing on microwave imagery. Amos subsequently peaked as a Category 3 Severe Tropical Cyclone, with ten-minute sustained wind speeds of during April 22. During that day as the cyclone passed within of Wallis Island, the JTWC estimated that Amos had peaked with 1-minute sustained winds of. Over the next day, the system remained at its peak intensity as it accelerated south-eastwards towards the Samoan Islands, where it was expected to pass over either Upolu or Tutuila. Amos subsequently continued its south-eastwards movement and was thought to have passed very close to or over the Samoan Islands during April 23. The system subsequently significantly weakened over the next day, as the circulation broke down and became sheared. The system subsequently degenerated into a tropical disturbance during April 25, before it was last noted near American Samoa's Manuʻa Islands.