Hurricane Jebi Track Map & Archive

Dissipated

Local time · Active from 25 Sep 2024 04:00 GMT+10 to 03 Oct 2024 05:00 GMT+11

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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
29.52Mpeople
🏥 Hospitals & Medical Centers
537facilities
🏕️ Evacuation Shelters & Centers
1640centers
🏫 Schools & Critical Infrastructure
3936buildings
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AI Historical Storm Matches

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

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Basic Information

Peak Category

Extratropical Cyclone

Minimum Pressure

972 hPa

Maximum Wind Speed

130 km/h

Region

West Pacific

Key Events

Formation

25 Sep 2024 04:00 GMT+10

14.3°N, 149.8°E

Dissipation

03 Oct 2024 05:00 GMT+11

52.3°N, 160.5°E

Frequently Asked Questions about Jebi

No, Jebi is no longer active. It dissipated or transitioned into an extratropical cyclone on 2024-10-02T18:00:00.000Z.
Jebi formed on 2024-09-24T18:00:00.000Z and dissipated on 2024-10-02T18:00:00.000Z, reaching a peak intensity of extratropical.

Storm Timeline

Jebi at 52.3°N, 160.5°E as Extratropical Cyclone with winds of 0 km/h

Jebi at 50.6°N, 158.3°E as Extratropical Cyclone with winds of 0 km/h

Jebi at 48.8°N, 156.6°E as Extratropical Cyclone with winds of 83 km/h (52 mph)

Jebi at 46.9°N, 154.7°E as Tropical Storm with winds of 86 km/h (53 mph)

Jebi at 45.1°N, 152.8°E as Tropical Storm with winds of 90 km/h (56 mph)

Jebi at 43.5°N, 150.7°E as Tropical Storm with winds of 108 km/h (67 mph)

Jebi at 42.1°N, 148.7°E as Tropical Storm with winds of 108 km/h (67 mph)

Jebi at 40.6°N, 147.0°E as Category 1 (equivalent to Category 1 Hurricane) with winds of 130 km/h (81 mph)

Jebi at 39.2°N, 145.5°E as Category 1 (equivalent to Category 1 Hurricane) with winds of 119 km/h (74 mph)

Jebi at 38.0°N, 144.3°E as Category 1 (equivalent to Category 1 Hurricane) with winds of 130 km/h (81 mph)

Typhoon Jebi 2024: A Rare Open-Ocean Storm That Spared Japan’s Coast

Typhoon Jebi 2024 evolved from a tropical depression over the western Pacific into a typhoon while remaining far from major land areas in East Asia. The storm reached its peak intensity on October 1 east of Japan, with maximum sustained winds of 65 knots and a central pressure of 980 hPa in the official Japan Meteorological Agency best-track record. Jebi later weakened over the North Pacific before becoming an extratropical cyclone on October 2. The storm’s history demonstrated the interaction between tropical systems and the mid-latitude environment across the western Pacific.

Mariana Islands Genesis: Jebi’s Northwest Track Across Open Pacific

Jebi began developing on September 25, 2024, over the western Pacific near the Mariana Islands as a tropical depression. The system formed east of the Philippines and south of Japan, where warm ocean waters supported gradual organization of its circulation. After formation, Jebi moved generally northwestward through the open Pacific while slowly gaining strength.

During its early development, the cyclone passed east of the Mariana Islands and approached the region around the Ogasawara Islands, also known as the Bonin Islands. On September 26, the system strengthened into a tropical storm under the regional classification system used for western Pacific monitoring. The system experienced sporadic intensity fluctuations as its circulation adjusted to changing atmospheric conditions.

Jebi continued tracking northward across the Pacific east of Japan’s southern islands. The storm remained offshore and did not approach major population centers along Honshu, Japan’s largest island, or the nearby island communities. Forecast agencies continued tracking its movement because western Pacific cyclones can influence marine conditions and coastal weather patterns even without direct landfall.

The storm was officially designated Typhoon No. 17 (T2417) by Japan’s meteorological authorities during its mature phase. Under the Japanese classification system, Jebi progressed from a tropical depression into a tropical storm before reaching typhoon intensity over open waters east of Japan. Its track kept the strongest part of the circulation away from the Japanese coastline.

Peak Intensity East of Japan: Rapid Acceleration and Offshore Typhoon Transition

Jebi entered its strongest phase at the beginning of October as it moved northeastward over the Pacific east of Japan. On September 30, the system strengthened while located near 28.5°N and 140.8°E, then intensified into a typhoon on October 1.

The official best-track analysis recorded Jebi’s peak intensity at 0000 UTC on October 1, when the storm was positioned near 32.7°N and 141.6°E. The typhoon reached maximum sustained winds of 65 knots with a central pressure of 980 hPa. This intensity placed Jebi within the typhoon category while following a predominantly oceanic path.

At its strongest stage, Jebi moved through waters east of the Japanese archipelago rather than toward the coastline. The storm passed well away from the main islands, including Honshu, while maintaining a northeastward trajectory toward the higher latitudes of the North Pacific.

For Japan, operational attention focused on offshore wind, wave conditions, and potential indirect effects rather than a direct landfall threat. Coastal regions and marine operators tracked the system because strong winds and high waves associated with distant typhoons can affect shipping routes and ocean conditions.

The storm’s movement also brought it closer to the transition zone between tropical and mid-latitude weather systems. Cooler waters, stronger upper-level winds, and changing atmospheric conditions gradually weakened the tropical structure after Jebi reached its peak intensity.

Beyond Japan’s Waters: Extratropical Transition Over the North Pacific

After reaching peak strength, Jebi accelerated toward the northeast and began losing tropical characteristics. By October 2, the storm had weakened to tropical storm intensity while moving across the open North Pacific near the region east of the Kuril Islands.

Such extratropical transitions are a familiar outcome for western North Pacific storms that migrate into higher latitudes. As these systems leave tropical environments, they often interact with frontal boundaries and the broader mid-latitude circulation, changing from warm-core tropical cyclones into larger extratropical weather systems.

Jebi completed its transition into an extratropical cyclone on October 2 near 52.3°N and 160.5°E. The former typhoon then continued within the North Pacific extratropical environment before eventually dissipating.

Although Jebi did not produce a major land disaster in Japan, China, the Philippines, or Vietnam, its offshore track demonstrated the value of persistent tracking for western Pacific storms. A cyclone can remain distant from land while still affecting marine forecasting, regional weather patterns, and operational planning across East Asia.

Jebi’s 2024 Track: What an Offshore Typhoon Taught Pacific Forecasters

Jebi’s 2024 journey represented a classic recurving western Pacific typhoon pattern. The storm formed near the Mariana Islands, traveled across the open Pacific, strengthened east of Japan, and transitioned into an extratropical cyclone after entering higher latitudes.

The system was part of the western North Pacific typhoon season monitored by regional forecasting centers across East Asia. Its development and movement provided additional operational data for analyzing cyclone formation, intensity changes, and interactions between tropical and extratropical environments.

The storm also reflected the challenges of forecasting offshore typhoons. While Jebi avoided direct impacts on densely populated coastal areas, its evolution required accurate tracking of wind structure, pressure changes, and movement across a large ocean basin.

During the 2024 season, the Japan Meteorological Agency continued refining its forecasting and monitoring capabilities while maintaining detailed records of tropical cyclone activity. Jebi’s official track remains documented as a storm that reached typhoon strength east of Japan before completing extratropical transition over the North Pacific.