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Cyclone Chido

South-West Indian Ocean cyclone in 2024

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Intense Tropical Cyclone Chido on 12 December 2024
VIIRS imagery from NOAA's NOAA-21 Satellite · Public domain

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Through Atmospheric pressure

Chido originated from an elongated circulation that the Météo-France office in Réunion (RSMC La Réunion) began monitoring on 7 December, located east of Diego Garcia. In the post-storm analysis, it was indicated that the storm had already begun forming as a zone of disturbed weather on 5 December. On 11 December, Chido rapidly deepened and intensified into an intense tropical cyclone within twelve hours, with its eye passing over Agaléga. Early the next day, the United States Joint Typhoon Warning Center (JTWC) upgraded the system to a Category 4-equivalent tropical cyclone, with estimated 1-minute maximum sustained winds of 250 km/h (155 mph), while the MFR estimated its peak intensity with a minimum central pressure of 935 hPa (27.61 inHg) and 10-minute maximum sustained winds of 215 km/h (130 mph) as it maintained its small size and moved westwards. As the system passed off the northern tip of Madagascar, the eye briefly cleared and the central dense overcast remained compact and symmetrical. Chido entered the Mozambique Channel on 14 December, with microwave imagery showing highly developed organized bands of deep convection. Satellite imagery showed cooling cloud tops surrounding a clearing eye, indicating the strengthening of the storm, and on 15 December, Chido made landfall in Pemba, Mozambique, with 10-minute sustained winds estimated at 205 km/h (125 mph). Shortly after landfall, the MFR reported that Chido moved through Mozambique and Malawi, with convective activity gradually weakening. On 16 December, Chido degenerated into an overland depression, and the MFR issued its final advisory on the system.

The deaths of at least 173 people are attributed to Chido; 120 in Mozambique, 40 in Mayotte and 13 in Malawi, along with over 5,194 injuries. Agaléga was significantly affected by Chido, with over 95% of the territory's buildings destroyed. Little was done to prepare for the storm in Mayotte, which experienced catastrophic damage and a heavily debated number of deaths and missing from Chido. Numerous residents were unaccounted for, with most shanty towns completely destroyed and 85% of the island being left without power by 16 December. In Mozambique, over 155,500 homes were badly affected and entire communities were destroyed. Relatively minor damage also occurred in the Comoros and Madagascar. Economic losses from Chido reached $3.9 billion, making it the costliest tropical cyclone in the South-West Indian Ocean basin.

Meteorological history

Cyclone Chido originated from an elongated circulation that the Météo-France office in Réunion (MFR) began monitoring on 7 December, located east of Diego Garcia. In the post-storm analysis, it was indicated that the storm had already begun forming as a zone of disturbed weather on 5 December. On 8 December, at 08:00 UTC, the United States Joint Typhoon Warning Center (JTWC) issued a tropical cyclone formation alert, noting a consolidating low-level circulation center and a favorable environment with low wind shear and sea surface temperatures exceeding 28–29 °C (82–84 °F). The following day, the JTWC began issuing warnings for the system, classifying it as Tropical Cyclone 04S, as satellite imagery showed a partially exposed low-level circulation center on the eastern side of a developing burst of deep convection, which was nearly circular in shape and had cloud tops cooler than −80 °C (−112 °F). At 00:00 UTC on 10 December, the MFR reported that the system had intensified into a moderate tropical storm, with the Mauritius Meteorological Services naming it Chido, as convection strongly increased around the center of the system, accompanied by cooling of cloud tops and an expansion of the central dense overcast (CDO). The cyclone moved westward, and the MFR reported that it quickly intensified into a severe tropical storm around 12:00 UTC that day, citing the Dvorak technique—a method used to determine a tropical cyclone's intensity based on its satellite appearance. On the subsequent day, Chido significantly improved in organization, with satellite imagery showing a newly developed eye feature, an increasingly symmetric structure, and curved convective banding wrapping around the system. As a result, MFR upgraded it to a tropical cyclone, and the JTWC followed suit.

Chido rapidly deepened and intensified into an intense tropical cyclone within twelve hours, with its eye passing over Agalega and bringing extreme conditions to the island, where a minimum pressure of 980 hPa (28.94 inHg) was recorded. This made Chido the strongest tropical cyclone to directly affect the island since Cyclone Andry in 1983. Early the next day, the JTWC upgraded the system to a Category 4-equivalent tropical cyclone, with estimated 1-minute maximum sustained winds of 250 km/h (155 mph), while the MFR estimated its peak intensity with a minimum central pressure of 935 hPa (27.61 inHg) and 10-minute maximum sustained winds of 215 km/h (130 mph) as it maintained its small size and moved westwards. After reaching its peak intensity, the cyclone's eye, which was 13.8 miles (22.2 km) wide, became cloud-filled and increasingly ragged, and on 13 December, an eyewall replacement cycle occurred, causing the storm to weaken. As the system passed about 35 nautical miles (64.8 km) off the northern tip of Madagascar, the eye briefly cleared and the CDO remained compact and symmetrical. Chido entered the Mozambique Channel on 14 December, with microwave imagery showing highly developed organized bands of deep convection. As it neared Mayotte, it quickly re-intensified, with Pamandzi Airport recording a maximum gust of 226 km/h (140 mph), setting an all-time record for the station, and a minimum pressure of 982 hPa (29.00 inHg), breaking the previous record of 985 hPa (29.09 inHg) set during Cyclone Kamisy in 1984. Additionally, the MFR reported that it was the strongest storm to strike Mayotte in at least 90 years. Satellite imagery showed cooling cloud tops surrounding a clearing eye, indicating the strengthening of the storm, and at 06:00 UTC on 15 December, Chido made landfall on Pemba in Mozambique, with 10-minute sustained winds estimated at 205 km/h (125 mph). Shortly after landfall, the JTWC discontinued warnings, and the MFR reported that Chido moved through Mozambique and Malawi, with convective activity gradually weakening. On 16 December, Chido degenerated into an overland depression, and the MFR issued its final advisory on the system.

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