2014 Western Pacific typhoon season

Typhoon Halong 2014

Halong reached Category 5 strength east of the Philippines before turning toward Japan. Changes to its eyewall interrupted the powerful phase, and it arrived on Shikoku as a tropical storm.

PEAK INTENSITYCategory 5
Halong 2014: HALONG infrared satellite image, 2014-08-02T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
HALONG: complete recorded track, Jul 27, 2014–Aug 15, 2014Recorded track from Jul 27, 2014 to Aug 15, 2014. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAASIAINDIATAIWANFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanJul 28, 12:00 AM UTCJul 29, 12:00 AM UTCJul 30, 12:00 AM UTCJul 31, 12:00 AM UTCAug 1, 12:00 AM UTCAug 2, 12:00 AM UTCAug 3, 12:00 AM UTCAug 4, 12:00 AM UTCAug 5, 12:00 AM UTCAug 6, 12:00 AM UTCAug 7, 12:00 AM UTCAug 8, 12:00 AM UTCAug 9, 12:00 AM UTCAug 10, 12:00 AM UTCAug 11, 12:00 AM UTCAug 12, 12:00 AM UTCAug 13, 12:00 AM UTCAug 14, 12:00 AM UTCAug 15, 12:00 AM UTCPeak: Category 5JUL 27AUG 15

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 918 mb
09001009602001020mphmbJul 27Aug 2Aug 8Aug 15
Forward speed 7 mphCumulative ACE 9.59 10⁴ kt²
0020204040mph10⁴ kt²Jul 27Aug 2Aug 8Aug 15
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure918 hPa

Aug 2, 2014 during the tropical stage

Recorded track duration18.25 days

Full archive record, including non-tropical stages if present

Approximate track distance4,400 mi

Along the recorded center positions

STORM HISTORY

Rapid intensification after Guam

Halong developed near Chuuk in late July, initially moving little before becoming a named storm on July 29. Its developing circulation brought strong winds to Guam. The cyclone then strengthened rapidly over the western Pacific, reaching archived sustained winds of 140 knots on August 2.

An eyewall replacement cycle weakened Halong after its peak. The core later reorganized and briefly strengthened again, but the storm lost intensity as it approached Japan. It was known as Jose while in the Philippine monitoring area.

Across Shikoku and beyond Japan

Halong weakened to a tropical storm before making landfall on Shikoku on August 10. It crossed southern Japan and became extratropical on August 11. The remaining circulation continued toward Siberia, where another developing system absorbed it near the end of the archived track on August 15.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Halong (2014)

QUICK ANSWERS

Halong in brief

What was Typhoon Halong's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Aug 2, 2014, 12:00 PM UTC.

What category was Typhoon Halong?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Aug 2, 2014, 12:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Halong's lowest pressure?

918 mb, the minimum central pressure recorded during its tropical stage, on Aug 2, 2014, 12:00 PM UTC.

When did Typhoon Halong occur?

The archived track runs from Jul 27, 2014, 06:00 PM UTC to Aug 15, 2014, 12:00 AM UTC, with the tropical stage from Jul 28, 2014, 06:00 AM UTC to Aug 10, 2014, 09:00 PM UTC.

Where did Typhoon Halong form?

In the Western Pacific basin, in the 2014 season. Its first archived position is 11.7°N, 151.6°E on Jul 27, 2014, 06:00 PM UTC.

Did Typhoon Halong make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 63 mph on Aug 10, 2014, 12:00 AM UTC. Positions are six-hourly, so this is not a landfall chronology.

METHODOLOGY

Data sources and limitations

The map and summary are generated from NOAA's IBTrACS v04r01 archive. Wind and category use US-agency records; minimum pressure is calculated during the tropical stage, with the archive's pressure source retained. Category 5 refers to the Saffir–Simpson one-minute wind scale; local agencies may use different classifications. Coastlines use Natural Earth's 1:10m land data.

Track distance adds great-circle distances between consecutive observations, excluding gaps over 12 hours. This track has no gaps over 12 hours. The line shows the storm's center, not its size, rainfall or flood extent. Converted wind speeds are rounded to the nearest whole unit.

Archive retrieved

NOAA IBTrACS archive and Field documentation

Sources & methodology