1967 Western Pacific typhoon season

Typhoon Opal 1967

Typhoon Opal spent almost three weeks over the western Pacific in 1967. After reaching Category 5 strength far from land, it followed a winding course south of Japan before turning northeast into higher latitudes.

PEAK INTENSITYCategory 5
OPAL: complete recorded track, Aug 29, 1967–Sep 19, 1967Recorded track from Aug 29, 1967 to Sep 19, 1967. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANPHILIPPINESTAIWANPacific OceanAug 29, 12:00 AM UTCAug 30, 12:00 AM UTCAug 31, 12:00 AM UTCSep 1, 12:00 AM UTCSep 2, 12:00 AM UTCSep 3, 12:00 AM UTCSep 4, 12:00 AM UTCSep 5, 12:00 AM UTCSep 6, 12:00 AM UTCSep 7, 12:00 AM UTCSep 8, 12:00 AM UTCSep 9, 12:00 AM UTCSep 10, 12:00 AM UTCSep 11, 12:00 AM UTCSep 12, 12:00 AM UTCSep 13, 12:00 AM UTCSep 14, 12:00 AM UTCSep 15, 12:00 AM UTCSep 16, 12:00 AM UTCSep 17, 12:00 AM UTCSep 18, 12:00 AM UTCSep 19, 12:00 AM UTCPeak: Category 5AUG 29SEP 19

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 178 mphPressure 930 mb
09201009702001020mphmbAug 29Sep 5Sep 12Sep 19
Forward speed 13 mphCumulative ACE 15.91 10⁴ kt²
0015303060mph10⁴ kt²Aug 29Sep 5Sep 12Sep 19
Maximum sustained wind178 mph

178 mph

Minimum recorded pressure920 hPa

Sep 4, 1967 during the tropical stage

Recorded track duration21 days

Full archive record, including non-tropical stages if present

Approximate track distance4,410 mi

Along the recorded center positions

STORM HISTORY

A long westward journey

The archived track begins north of the Marshall Islands on 29 August. Opal moved west-northwest and strengthened, reaching peak one-minute winds of 155 kt on 3 September. Its strongest phase occurred over open water, well east of the Mariana Islands.

Opal weakened as it continued northwest toward the seas south of Japan. Its course then flattened westward and briefly bent southwest near the Ogasawara Islands. It retained typhoon winds through this change in direction rather than immediately accelerating northeast.

A broad turn south of Japan

The storm finally turned north and then northeast south of Honshu. Its winds declined as it moved east of Japan, and the tropical stage ended on 17 September. Later positions continue across the northern Pacific through 19 September. No archived center position lies over land.

Further reading

NOAA IBTrACS v04r01 historical track archive

QUICK ANSWERS

Opal in brief

What was Typhoon Opal's highest wind speed?

178 mph, the highest one-minute sustained wind in its tropical stage, recorded on Sep 3, 1967, 12:00 PM UTC.

What category was Typhoon Opal?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Sep 3, 1967, 12:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Opal's lowest pressure?

920 mb, the minimum central pressure recorded during its tropical stage, on Sep 4, 1967, 12:00 AM UTC.

When did Typhoon Opal occur?

The archived track runs from Aug 29, 1967, 12:00 AM UTC to Sep 19, 1967, 12:00 AM UTC, with the tropical stage from Aug 29, 1967, 12:00 PM UTC to Sep 17, 1967, 03:00 AM UTC.

Where did Typhoon Opal form?

In the Western Pacific basin, in the 1967 season. Its first archived position is 15°N, 170°E on Aug 29, 1967, 12:00 AM UTC.

Did Typhoon Opal make landfall?

No archived position places Typhoon Opal'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