About: Cyclone Cliff

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Tropical Cyclone Cliff was first noted as a weak tropical disturbance on April 1, 2007, within a trough of low pressure about 210 km (130 mi) to the southwest of Rotuma. Over the next couple of days the system drifted towards the southeast and Fiji, in an area of strong wind shear. During April 3, the system slightly accelerated, as it moved towards the south-southeast before the westerly wind shear around the system relaxed sufficiently to allow the depression to consolidate while it was located near Vanua Levu.

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  • Tropical Cyclone Cliff was first noted as a weak tropical disturbance on April 1, 2007, within a trough of low pressure about 210 km (130 mi) to the southwest of Rotuma. Over the next couple of days the system drifted towards the southeast and Fiji, in an area of strong wind shear. During April 3, the system slightly accelerated, as it moved towards the south-southeast before the westerly wind shear around the system relaxed sufficiently to allow the depression to consolidate while it was located near Vanua Levu. Early on April 4, the depression moved around the northeastern tip of Vanua Levu as bands of atmospheric convection rapidly developed and wrapped into the low level circulation center. At 0300 UTC while the system was located about 95 km (60 mi) to the south-southeast of Labasa, RSMC Nadi named the depression, Cliff after the system had developed into a category 1 tropical cyclone on the Australian tropical cyclone intensity scale. This was despite gale force winds not being present near the systems center, as required by the tropical cyclone operational plan for the region. After Cliff had been named gale-force winds rapidly developed near the center, as it continued to intensify and accelerate towards the south-southeast through the Lau group of islands. At around 0900 UTC on April 4, the United States Joint Typhoon Warning Center (JTWC) initiated advisories on the system and designated it as Tropical Cyclone 23P as it became a tropical storm. Over the next 24 hours Cliff continued to intensify, before the JTWC and RSMC Nadi reported during the next day, that Cliff had reached its peak intensity with sustained wind-speeds of 100 km/h (65 mph). After peaking in intensity, the system subsequently accelerated further towards the southeast and into an area of cooler seas and higher wind shear. This subsequently caused Cliff to become an extratropical cyclone during February 6, before the system was last noted later that day as it merged with a mid-latitude frontal boundary. Cyclone Cliff was responsible for one death. In the wake of the storm, an outbreak of typhoid and leptospirosis infected 99 people and killed three across Fiji. (en)
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  • Fiji and Tonga (en)
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  • SPac (en)
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  • 4 (xsd:integer)
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  • 2007-04-06 (xsd:date)
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  • 1 (xsd:integer)
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  • 2007-04-01 (xsd:date)
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  • Cliff 2007-04-05 0145Z.jpg (en)
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  • Tropical Cyclone Cliff at peak (en)
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  • Tropical Cyclone Cliff (en)
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  • 980 (xsd:integer)
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  • Tropical Storm (en)
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  • Tropical Cyclone Cliff was first noted as a weak tropical disturbance on April 1, 2007, within a trough of low pressure about 210 km (130 mi) to the southwest of Rotuma. Over the next couple of days the system drifted towards the southeast and Fiji, in an area of strong wind shear. During April 3, the system slightly accelerated, as it moved towards the south-southeast before the westerly wind shear around the system relaxed sufficiently to allow the depression to consolidate while it was located near Vanua Levu. (en)
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  • Cyclone Cliff (en)
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