1988 Western Pacific typhoon season

Typhoon Nelson 1988

Typhoon Nelson intensified rapidly over the Philippine Sea in October 1988 before turning northeast near Okinawa. Its center stayed offshore, but rain reached the island as the storm began weakening.

PEAK INTENSITYCategory 5
Nelson 1988: NELSON infrared satellite image, 1988-10-04T02:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
NELSON: complete recorded track, Sep 30, 1988–Oct 12, 1988Recorded track from Sep 30, 1988 to Oct 12, 1988. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAASIAINDIAFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanOct 1, 12:00 AM UTCOct 2, 12:00 AM UTCOct 3, 12:00 AM UTCOct 4, 12:00 AM UTCOct 5, 12:00 AM UTCOct 6, 12:00 AM UTCOct 7, 12:00 AM UTCOct 8, 12:00 AM UTCOct 9, 12:00 AM UTCOct 10, 12:00 AM UTCOct 11, 12:00 AM UTCOct 12, 12:00 AM UTCPeak: Category 5SEP 30OCT 12

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 915 mb
09001009602001020mphmbSep 30Oct 4Oct 8Oct 12
Forward speed 9 mphCumulative ACE 10.73 10⁴ kt²
003517.57035mph10⁴ kt²Sep 30Oct 4Oct 8Oct 12
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure915 hPa

Oct 4, 1988 during the tropical stage

Recorded track duration12.5 days

Full archive record, including non-tropical stages if present

Approximate track distance5,330 mi

Along the recorded center positions

STORM HISTORY

Rapid development after a quiet interval

Nelson formed within the monsoon trough after a lull in western Pacific cyclone activity. Its thunderstorms organized near the end of September, and it became a tropical storm on 1 October. Moving west and then west-northwest, it developed an eye and strengthened into a typhoon.

Rapid deepening brought Nelson to peak archived one-minute winds of 140 kt on 4 October. The storm then rounded the western edge of the subtropical ridge and accelerated northeast, beginning a gradual decline in intensity.

Passing southeast of Okinawa

Nelson passed about 155 km southeast of Okinawa, where 212 mm of rain was recorded. It rapidly lost deep convection as it moved away, transitioning into an extratropical cyclone by 9 October.

The archive follows Nelson's later circulation through 12 October. No recorded center position lies over land during its passage from the Philippine Sea into the northern Pacific.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 1988 Pacific typhoon season, Nelson section

QUICK ANSWERS

Nelson in brief

What was Typhoon Nelson's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Oct 4, 1988, 12:00 PM UTC.

What category was Typhoon Nelson?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Oct 4, 1988, 12:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Nelson's lowest pressure?

915 mb, the minimum central pressure recorded during its tropical stage, on Oct 4, 1988, 06:00 AM UTC.

When did Typhoon Nelson occur?

The archived track runs from Sep 30, 1988, 06:00 AM UTC to Oct 12, 1988, 06:00 PM UTC, with the tropical stage from Sep 30, 1988, 06:00 AM UTC to Oct 8, 1988, 09:00 PM UTC.

Where did Typhoon Nelson form?

In the Western Pacific basin, in the 1988 season. Its first archived position is 11.8°N, 141.7°E on Sep 30, 1988, 06:00 AM UTC.

Did Typhoon Nelson make landfall?

No archived position places Typhoon Nelson's center over land, but positions are six-hourly and a brief landfall can fall between them.

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