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Cyclone Dineo

South-West Indian Ocean tropical cyclone in 2017

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Meteorological history

The origins of Dineo can be tracked back to a cluster of thunderstorms that organized into an area of low pressure in the Mozambique Channel on 11 February. Over the next two days, the system gradually drifted in a generally southern track as it gained intensity and prompted the JTWC to issue a TCFA. On 13 February, RSMC La Réunion declared that a Tropical Disturbance had formed in the area and began issuing advisories. Located in a very favorable environment, the depression quickly increased in intensity and both the RSMC and JTWC noted winds of at least 65 km/h (40 mph) later that day, with the RSMC subsequently naming the storm Dineo. Dineo intensified to a tropical cyclone later on. It reached its peak intensity with maximum sustained winds of 85 mph (140 km/h) and a low barometric pressure of 955 hPa (mbar); 28.20 inHg on 15 February. Dineo made landfall on the coast of Mozambique, and it started weakening after landfall on the same day. On 17 February after making landfall, the JTWC issued the final advisory on Dineo. Dineo later dissipated after a few hours on the same day.

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