Major Hurricane Sinlaku Track Map & Archive

Dissipated

Local time · Active from 09 Apr 2026 10:00 GMT+10 to 20 Apr 2026 11:00 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
13.84Mpeople
🏥 Hospitals & Medical Centers
252facilities
🏕️ Evacuation Shelters & Centers
769centers
🏫 Schools & Critical Infrastructure
1846buildings

Basic Information

Peak Category

Tropical Storm

Minimum Pressure

896 hPa

Maximum Wind Speed

284 km/h

Region

West Pacific

Key Events

Formation

09 Apr 2026 10:00 GMT+10

8.7°N, 152.1°E

Dissipation

20 Apr 2026 11:00 GMT+11

29.6°N, 158.8°E

Frequently Asked Questions about Sinlaku

No, Sinlaku is no longer active. It dissipated or transitioned into an extratropical cyclone on 2026-04-20T00:00:00.000Z.
Sinlaku formed on 2026-04-09T00:00:00.000Z and dissipated on 2026-04-20T00:00:00.000Z, reaching a peak intensity of tropical_storm.

Storm Timeline

Sinlaku at 29.6°N, 158.8°E as Tropical Storm with winds of 94 km/h (58 mph)

Sinlaku at 29.1°N, 157.4°E as Tropical Storm with winds of 94 km/h (58 mph)

Sinlaku at 28.7°N, 156.1°E as Tropical Storm with winds of 94 km/h (58 mph)

Sinlaku at 28.5°N, 154.9°E as Tropical Storm with winds of 97 km/h (60 mph)

Sinlaku at 28.3°N, 153.7°E as Tropical Storm with winds of 97 km/h (60 mph)

Sinlaku at 28.0°N, 152.5°E as Tropical Storm with winds of 97 km/h (60 mph)

Sinlaku at 27.6°N, 151.4°E as Tropical Storm with winds of 94 km/h (58 mph)

Sinlaku at 27.1°N, 150.4°E as Tropical Storm with winds of 97 km/h (60 mph)

Sinlaku at 26.5°N, 149.5°E as Tropical Storm with winds of 97 km/h (60 mph)

Sinlaku at 25.9°N, 148.9°E as Tropical Storm with winds of 97 km/h (60 mph)

Super Typhoon Sinlaku 2026: 185-mph Category 5 Storm Strikes Mariana Islands

Super Typhoon Sinlaku had become the strongest tropical cyclone of 2026 up to that point after undergoing explosive intensification over the western North Pacific in early April. The system formed from a tropical disturbance on April 8, 2026, became a tropical depression on April 9, and later reached peak Category 5 intensity with maximum winds of 185 mph (160 kt, 295 km/h) and a minimum central pressure near 890 hPa. Sinlaku crossed the Mariana Islands region as a powerful major typhoon, bringing destructive winds, flooding, and widespread damage to Saipan, Tinian, Guam, and nearby islands. The cyclone transitioned into an extratropical system on April 20 before fully dissipating over the North Pacific on April 22.

Birth Near Micronesia: Sinlaku’s Rapid Rise Across the Western Pacific

Sinlaku developed from a tropical disturbance near Micronesia on April 8, 2026, in the western North Pacific basin. The system entered official tropical cyclone monitoring after organizing near 8.7°N, 152.1°E and strengthening into a tropical depression at 00:00 UTC on April 9. Initial conditions showed a developing circulation with maximum winds of 28 mph and a central pressure of 1000 hPa.

The cyclone gained organization as convection increased around the center. At 21:00 UTC on April 9, Sinlaku strengthened into a tropical storm near 8.3°N, 151.4°E, with winds reaching 42 mph and pressure falling to 994 hPa. The storm continued moving through a favorable western Pacific environment, allowing its circulation to expand and its inner structure to become increasingly defined.

Sinlaku intensified further on April 10. At 18:00 UTC, the storm reached winds of 69 mph with a central pressure of 983 hPa while remaining east of the Mariana Islands. The strengthening rate accelerated during the following day, and the cyclone reached Category 2-equivalent intensity at 15:00 UTC on April 11, producing winds of 102 mph and a pressure of 961 hPa.

The most dramatic phase of Sinlaku’s development occurred between April 11 and April 12. The cyclone rapidly strengthened into a Category 5-equivalent super typhoon while positioned over open Pacific waters. At 12:00 UTC on April 12, Sinlaku reached winds of 170 mph with a pressure of 902 hPa near 11.1°N, 150.2°E. Six hours later, the storm reached its peak near 11.6°N, 149.5°E with maximum sustained winds of 185 mph and a minimum pressure of approximately 890 hPa.

The name Sinlaku originates from a legendary goddess associated with Kosrae, one of the islands of the Federated States of Micronesia. The designation reflects the regional naming tradition used for western Pacific tropical cyclones, where names are contributed by countries and territories around the basin.

Category 5 Peak Over Open Waters: Sinlaku’s 890 hPa Intensity Milestone

At peak strength, Sinlaku ranked among the most intense tropical cyclones observed in the western North Pacific during 2026. The storm maintained a highly organized structure with a distinct eye and intense convection surrounding the core as it approached the Mariana Islands.

Different meteorological datasets reported slight variations in the cyclone’s peak intensity. Japanese Meteorological Agency records using a 10-minute averaging standard placed the storm near 215 km/h winds and around 905 hPa, while other operational estimates based on the Joint Typhoon Warning Center and satellite intensity analysis recorded higher one-minute sustained winds near 185 mph and pressure around 890 hPa. These differences reflect the separate measurement methods used by international forecasting agencies.

The rapid intensification phase compressed the forecasting window for impact assessments as Sinlaku strengthened from a tropical storm into a Category 5-equivalent system within a short period. Forecast centers monitored changes in track, intensity, and potential effects on Guam and the Northern Mariana Islands as the storm moved westward.

Sinlaku remained near peak intensity into April 13. At 09:00 UTC, the typhoon was still producing winds near 170 mph and a central pressure of about 903 hPa near 12.9°N, 147.7°E. The cyclone then began a gradual weakening trend as it moved closer to land and interacted with less favorable conditions.

By 06:00 UTC on April 14, Sinlaku had weakened to a Category 4-equivalent typhoon near 14.6°N, 146.0°E. Winds decreased to 147 mph while pressure rose to 925 hPa, but the system remained capable of producing severe impacts across the Mariana Islands.

Mariana Islands Impact Zone: Sinlaku’s Destructive Passage Through Guam and Saipan

Sinlaku affected the Mariana Islands while still maintaining major typhoon intensity. Saipan and Tinian experienced some of the strongest conditions as the cyclone passed through the region, with destructive winds, intense rainfall, and coastal hazards affecting communities and infrastructure.

Saipan International Airport recorded a wind gust of 130 mph during the height of the storm. Guam International Airport measured a peak gust near 88 mph. The strongest winds damaged buildings, disrupted transportation services, and caused widespread power interruptions across affected islands.

The cyclone’s rainfall created significant flooding problems, particularly in areas exposed to prolonged heavy precipitation. Emergency agencies in Guam and the Northern Mariana Islands coordinated storm response activities, including damage assessments, restoration of essential services, and support for residents affected by the typhoon.

Sinlaku weakened while moving through the Mariana region. At 03:00 UTC on April 15, the storm was classified as a Category 3-equivalent typhoon near 15.8°N, 145.1°E, with winds of 125 mph and a pressure of 944 hPa. Despite the decline from its record-setting peak, the cyclone retained a dangerous wind field and continued producing hazardous weather.

The storm continued northward after leaving the islands. At 00:00 UTC on April 16, Sinlaku remained a Category 3-equivalent system near 17.1°N, 144.4°E with winds of 113 mph and a pressure of 955 hPa. Later that day, intensity dropped to Category 1-equivalent strength as the cyclone moved farther away from the Mariana Islands.

Dissipation Over the Pacific: Sinlaku’s Final Track and Meteorological Legacy

Sinlaku continued weakening after its passage through the western Pacific island chain. At 21:00 UTC on April 16, the storm was located near 19.3°N, 145.2°E with winds of 94 mph and a central pressure of 969 hPa. The cyclone maintained tropical characteristics while moving into a less favorable environment.

On April 17, Sinlaku remained a Category 1-equivalent tropical cyclone before weakening into a tropical storm. The system was positioned near 21.3°N, 146.5°E at 18:00 UTC, with winds of 80 mph and a pressure of 974 hPa.

The weakening trend continued over the following days. At 15:00 UTC on April 18, Sinlaku was a tropical storm near 24.8°N, 148.0°E with winds of 65 mph and a pressure of 982 hPa. On April 19, the cyclone moved farther northeast near 28.3°N, 153.7°E while maintaining tropical storm strength.

Sinlaku transitioned into an extratropical cyclone on April 20 near the western North Pacific, ending its tropical cyclone phase. The system later dissipated completely on April 22 after moving over open waters.

The record of Super Typhoon Sinlaku highlights the rapid intensity changes possible in the western Pacific basin. Its evolution from a developing disturbance near Micronesia to a Category 5-equivalent typhoon with winds of 185 mph and pressure near 890 hPa made it one of the most significant tropical cyclones of 2026. Its track, intensity changes, and impacts across the Mariana Islands remain documented through international meteorological monitoring systems.