Major Hurricane Djoungou Track Map & Archive

Dissipated

Local time · Active from 13 Feb 2024 10:00 GMT+4 to 20 Feb 2024 13:00 GMT+7

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Estimated Storm Impact Analysis

Real-time analysis of population and infrastructure exposure within the storm's wind field.

Radius: ~600 km
👥 Estimated Population at Risk
13.84Mpeople
🏥 Hospitals & Medical Centers
252facilities
🏕️ Evacuation Shelters & Centers
769centers
🏫 Schools & Critical Infrastructure
1846buildings
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AI Historical Storm Matches

Compare historical storms by track, pressure changes, and rapid intensification patterns.

AI Trajectory Match
Freddy84% Similarity Score
MAX: 248 m/s
MIN: 930 hPa
Rapid Intensification Risk:High Risk
View Historical Storm Track
Fabien71% Similarity Score
MAX: 191 m/s
MIN: 962 hPa
Rapid Intensification Risk:High Risk
View Historical Storm Track
Megan70% Similarity Score
MAX: 166 m/s
MIN: 950 hPa
Rapid Intensification Risk:High Risk
View Historical Storm Track

Basic Information

Peak Category

Extratropical Cyclone

Minimum Pressure

923 hPa

Maximum Wind Speed

259 km/h

Region

West Pacific

Key Events

Formation

13 Feb 2024 10:00 GMT+4

-13.7°N, 66.1°E

Dissipation

20 Feb 2024 13:00 GMT+7

-32.3°N, 100.5°E

Frequently Asked Questions about Djoungou

No, Djoungou is no longer active. It dissipated or transitioned into an extratropical cyclone on 2024-02-20T06:00:00.000Z.
Djoungou formed on 2024-02-13T06:00:00.000Z and dissipated on 2024-02-20T06:00:00.000Z, reaching a peak intensity of extratropical.

Storm Timeline

Djoungou at 32.3°S, 100.5°E as Extratropical Cyclone with winds of 90 km/h (56 mph)

Djoungou at 31.7°S, 97.8°E as subtropical with winds of 90 km/h (56 mph)

Djoungou at 30.8°S, 95.4°E as Tropical Storm with winds of 90 km/h (56 mph)

Djoungou at 30.1°S, 93.3°E as Tropical Storm with winds of 97 km/h (60 mph)

Djoungou at 29.3°S, 91.5°E as Tropical Storm with winds of 101 km/h (63 mph)

Djoungou at 28.2°S, 89.9°E as Category 1 (equivalent to Category 1 Hurricane) with winds of 126 km/h (78 mph)

Djoungou at 27.1°S, 88.4°E as Category 1 (equivalent to Category 1 Hurricane) with winds of 137 km/h (85 mph)

Djoungou at 26.0°S, 86.8°E as Category 2 (equivalent to Category 2 Hurricane) with winds of 155 km/h (96 mph)

Djoungou at 25.1°S, 85.5°E as Category 2 (equivalent to Category 2 Hurricane) with winds of 166 km/h (103 mph)

Djoungou at 24.2°S, 84.3°E as Category 3 (equivalent to Category 3 Hurricane) with winds of 180 km/h (112 mph)

Djoungou’s Record-Breaking Strength Defined a Fierce Indian Ocean Cyclone

Tropical Cyclone Djoungou developed in the southwestern Indian Ocean on 13 February 2024 and became one of the most intense cyclones of the 2023–2024 season. The storm reached its peak on 18 February over open waters near 19.2°S and 77.5°E, with JTWC reporting maximum one-minute sustained winds of 259 km/h and IBTrACS recording a minimum central pressure of 923. The cyclone remained offshore throughout its lifetime and did not make landfall in Madagascar, Australia, India, or the South Pacific island region. Djoungou completed its tropical phase on 20 February before transitioning into an extratropical system over the southern Indian Ocean.

Formation Over Open Waters: Djoungou’s Path From Depression to Named Cyclone

Djoungou began as a tropical depression on 13 February 2024 in the southwestern Indian Ocean, forming near 13.7°S and 66.1°E. The initial disturbance had maximum winds of approximately 27 km/h and a central pressure near 1010. Under favorable oceanic and atmospheric conditions, the circulation gradually strengthened as convection became better organized.

The system moved generally eastward and southeastward while remaining far from the coastlines of Madagascar and other populated islands. By 15 February, Djoungou had intensified into a tropical storm, with winds increasing to about 64 km/h and pressure falling to 997. The strengthening continued during the following day as wind speeds reached around 92 km/h.

Forecast operations during this period involved international monitoring networks, including the Regional Specialized Meteorological Centre (RSMC) La Réunion operated by Météo-France and the Joint Typhoon Warning Center (JTWC). These agencies tracked the cyclone’s position, intensity changes, and potential marine hazards across the southwestern Indian Ocean.

Although Djoungou never approached a populated coastline closely enough to produce a direct land impact, the storm remained significant for maritime interests. Strong tropical cyclones over the Indian Ocean can create dangerous waves, rough seas, and disrupted shipping conditions across large areas, affecting vessels traveling between Africa, Madagascar, India, Australia, and island territories.

The cyclone’s early development underscored the rapid changes that can occur in tropical systems. From 13 to 17 February, Djoungou strengthened from a weak depression into a Category 2-equivalent cyclone, with its pressure dropping from 1010 to 955 as the circulation became increasingly organized.

Peak Intensity Over the Indian Ocean: Djoungou Became a Very Intense Tropical Cyclone

Djoungou experienced its most dramatic intensification from 17 to 18 February 2024. The cyclone strengthened from a Category 2 system into a powerful major cyclone while moving through the open southwestern Indian Ocean.

On 18 February, Djoungou reached its maximum intensity. JTWC estimated one-minute sustained winds of 259 km/h, equivalent to 140 knots, while the IBTrACS dataset recorded a minimum central pressure of 923. Some historical archives list slightly different pressure values, including 920 or 922, reflecting differences among analysis agencies and best-track datasets.

From the perspective of Météo-France and RSMC La Réunion, Djoungou reached the classification of a Very Intense Tropical Cyclone, with ten-minute sustained winds estimated at approximately 215 km/h. The difference between JTWC and Météo-France wind values results from different averaging periods used by meteorological agencies: JTWC applies a one-minute average, while RSMC La Réunion uses a ten-minute average consistent with World Meteorological Organization regional standards.

The cyclone’s peak occurred far from Madagascar and other vulnerable island communities. No direct destructive landfall occurred, but the storm represented a major oceanic weather event during the regional cyclone season. Coastal areas in Madagascar, the Mascarene Islands, and other Indian Ocean locations remained outside the core wind field.

Djoungou was recognized as one of the strongest tropical cyclones of the 2023–2024 southwestern Indian Ocean season. Its rapid intensification phase showed how quickly a tropical cyclone can evolve when warm ocean waters, low wind shear, and favorable atmospheric conditions combine.

Final Track Across Southern Waters: Djoungou’s Shift Into an Extratropical Storm

After reaching peak intensity on 18 February, Djoungou began weakening as it moved toward higher southern latitudes. The cyclone encountered less favorable conditions, including cooler waters and changing atmospheric patterns, which reduced its tropical characteristics.

By 19 February, the storm had weakened from its peak strength, with winds decreasing to approximately 166 km/h and central pressure rising to 952. The system continued moving away from the tropical Indian Ocean region while maintaining a well-defined circulation.

On 20 February, Djoungou completed its transition into an extratropical system near 32.3°S and 100.5°E. At that stage, winds were around 92 km/h and the pressure was near 987. The storm no longer maintained the warm-core structure associated with tropical cyclones.

Because Djoungou remained over open waters, Madagascar avoided the severe wind and rainfall impacts often associated with major Indian Ocean cyclones. Australia, India, and South Pacific island communities also experienced no direct effects from the cyclone’s core circulation. The main recorded impacts were associated with ocean conditions and operational monitoring rather than widespread land damage.

Djoungou’s complete lifecycle, from tropical depression formation on 13 February to extratropical transition on 20 February, remains a documented example of rapid strengthening and offshore cyclone evolution in the southwestern Indian Ocean. Its track records, intensity measurements, and classification history continue to form part of international tropical cyclone archives.