1989 Western Pacific typhoon season

Typhoon Gordon 1989

Typhoon Gordon struck northern Luzon near peak strength in July 1989 and later brought severe flooding to southern China. Although weaker at its Chinese landfall, the storm caused its greatest reported loss of life there.

PEAK INTENSITYCategory 5
Gordon 1989: GORDON infrared satellite image, 1989-07-15T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
GORDON: complete recorded track, Jul 9, 1989–Jul 19, 1989Recorded track from Jul 9, 1989 to Jul 19, 1989. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANPHILIPPINESTAIWANFIJIVANUATUJul 9, 12:00 AM UTCJul 10, 12:00 AM UTCJul 11, 12:00 AM UTCJul 12, 12:00 AM UTCJul 13, 12:00 AM UTCJul 14, 12:00 AM UTCJul 15, 12:00 AM UTCJul 16, 12:00 AM UTCJul 17, 12:00 AM UTCJul 18, 12:00 AM UTCJul 19, 12:00 AM UTCPeak: Category 5JUL 9JUL 19

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 915 mb
09001009602001020mphmbJul 9Jul 12Jul 15Jul 19
Forward speed 13 mphCumulative ACE 9.53 10⁴ kt²
001512.53025mph10⁴ kt²Jul 9Jul 12Jul 15Jul 19
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure915 hPa

Jul 15, 1989 during the tropical stage

Recorded track duration10.25 days

Full archive record, including non-tropical stages if present

Approximate track distance3,640 mi

Along the recorded center positions

STORM HISTORY

Rapid strengthening toward Luzon

Gordon developed east of the Northern Mariana Islands and moved west-southwest beneath a subtropical ridge. It became a typhoon on 13 July and intensified rapidly. Peak archived one-minute winds reached 140 kt on 15 July.

The typhoon struck the northern Philippines and then crossed the South China Sea while gradually weakening. Ninety people died in the Philippines, and an estimated 120,000 were left homeless.

Severe flooding in southern China

Gordon reached southern China on 18 July. Extensive flooding inundated coastal cities and caused at least 200 deaths. Reported losses in China reached 1.2 billion yuan, equivalent to US$319 million in 1989 values.

Fourteen people also drowned offshore, and two deaths occurred in Hong Kong. Gordon weakened over land and was last tracked on 19 July, after a ten-day passage from the western Pacific to southern China.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Gordon (1989)

QUICK ANSWERS

Gordon in brief

What was Typhoon Gordon's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jul 15, 1989, 06:00 AM UTC.

What category was Typhoon Gordon?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Jul 15, 1989, 06:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Gordon's lowest pressure?

915 mb, the minimum central pressure recorded during its tropical stage, on Jul 15, 1989, 06:00 AM UTC.

When did Typhoon Gordon occur?

The archived track runs from Jul 9, 1989, 12:00 AM UTC to Jul 19, 1989, 06:00 AM UTC, with the tropical stage from Jul 9, 1989, 12:00 AM UTC to Jul 19, 1989, 06:00 AM UTC.

Where did Typhoon Gordon form?

In the Western Pacific basin, in the 1989 season. Its first archived position is 20°N, 160.2°E on Jul 9, 1989, 12:00 AM UTC.

Did Typhoon Gordon make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 150 mph on Jul 15, 1989, 09:00 PM 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