Typhoon Halong Track Map & Archive

Dissipated

Local time · Active from 03 Oct 2025 10:00 GMT+10 to 11 Oct 2025 00:00 GMT-12

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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

Extratropical Cyclone

Minimum Pressure

936 hPa

Maximum Wind Speed

220 km/h

Region

West Pacific

Key Events

Formation

03 Oct 2025 10:00 GMT+10

20.1°N, 147.4°E

Dissipation

11 Oct 2025 00:00 GMT-12

45.3°N, 182.2°E

Frequently Asked Questions about Halong

No, Halong is no longer active. It dissipated or transitioned into an extratropical cyclone on 2025-10-11T12:00:00.000Z.
Halong formed on 2025-10-03T00:00:00.000Z and dissipated on 2025-10-11T12:00:00.000Z, reaching a peak intensity of Extratropical Cyclone.

Key Meteorological Milestones

Synthesized from official bulletins (NHC/NOAA, JMA, CMA, KMA). Licensed for non-commercial educational & academic research.

🌀

Genesis & Initial Classification

Tropical Depression
📅 03 Oct 2025 00:00 (03 Oct 2025 10:00 GMT+10)🌐 20.1°N, 147.4°E🏛️ Official
Wind Speed-
Pressure1010 hPa
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Named Storm Upgrade (TS)

Tropical Storm
📅 04 Oct 2025 06:00 (04 Oct 2025 16:00 GMT+10)🌐 24.4°N, 143.7°E🏛️ Official
Wind Speed65 km/h (35 kt)
Pressure1000 hPa
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System Regeneration / Re-intensification

Tropical Depression
📅 04 Oct 2025 09:00 (04 Oct 2025 19:00 GMT+10)🌐 24.6°N, 143.6°E🏛️ Official
Wind Speed-
Pressure-
🏆

Peak Lifetime Intensity (LMI)

Category 3
📅 07 Oct 2025 18:00 (08 Oct 2025 03:00 GMT+9)🌐 28.8°N, 137.0°E🏛️ Official
Wind Speed184 km/h (99 kt)
Pressure935 hPa
📉 Pressure Drop-75 hPa
🌫️

Extratropical Transition (Post-Tropical)

Extratropical Cyclone
📅 11 Oct 2025 12:00 (11 Oct 2025 12:00 UTC)🌐 45.3°N, 182.2°E🏛️ Official
Wind Speed-
Pressure-

💾Best-Track Scientific Dataset Exporter

⚪ Official Final Consolidated Archive

Synthesized research-grade meteorological data ready for Excel, Python Pandas, or GIS platforms, compliant with academic citations and multi-agency validation.

Meteorological Retrospective & Hazard Analysis

Typhoon Halong (2025): A Retrospective on Life Cycle, Rapid Intensification, and Trans-Pacific Legacy

Introduction

Typhoon Halong (2025) stands as a stark reminder of the Western Pacific’s capacity to generate high-end tropical cyclones that retain destructive energy across thousands of kilometers. From its formation in the Philippine Sea to its ultimate demise as a catastrophic extratropical low over Alaska, Halong’s journey exemplified both the classical rapid-intensification regime and the often-underappreciated threat of post-tropical impacts. This report reconstructs the storm’s full life cycle, with emphasis on its intensity evolution, using official JTWC best-track data and satellite-derived analyses.

Rapid Intensification and Peak Intensity

October 7 marked the critical phase. Halong underwent explosive deepening. The storm’s central pressure plunged while its convective structure became remarkably symmetric.

| Parameter | Value |
|## Weakening and Extratropical Transition

After peak, Halong moved northeastward under increasing mid-latitude westerlies. The storm entered a region of higher vertical wind shear and cooler SSTs (<26°C). Two distinct phases of decay followed:

  1. Structural degradation (October 8–10): The eyewall eroded. Convective asymmetry became pronounced. The central pressure rose to 970 hPa by October 9. Winds dropped below typhoon force (64 kt) on October 10.

  2. Extratropical transition (October 11): Halong lost all tropical characteristics. The warm core collapsed; the system acquired a frontal structure. JTWC issued its final warning.

Yet the remnant low remained powerful. It accelerated toward the Gulf of Alaska, driven by a deep upper-level trough. The storm’s forward speed increased to 40–50 kt.

Summary of Key Metrics

| Event | Date (2025) | Winds (kt / mph) | Pressure (hPa) |
|-|-|-|## Conclusion

Halong (2025) demonstrates that a typhoon’s threat does not end at the mid-latitude boundary. The storm’s rapid intensification to a Category-4 equivalent — with 136-mph winds and 936-hPa central pressure — was both textbook and formidable. Yet its lasting legacy was the trans-Pacific journey that culminated in a major disaster thousands of kilometers from its tropical birthplace. For meteorological professionals, Halong reinforces the need to maintain vigilance during extratropical transition, especially when a former typhoon retains high-wind cores and abundant moisture. The 2025 season will be remembered for Halong’s intensity — and for the destruction it carried to the Arctic.