1963 Western Pacific typhoon season

Typhoon Shirley 1963

Typhoon Shirley curved north through the Philippine Sea in June 1963 before crossing the East China Sea toward Korea. It reached Category 5 strength east of the Philippines, then weakened along its northward route. The later track extends into the far northern Pacific.

PEAK INTENSITYCategory 5
SHIRLEY: complete recorded track, Jun 12, 1963–Jun 26, 1963Recorded track from Jun 12, 1963 to Jun 26, 1963. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAASIAINDIAFIJITONGAVANUATUNEW CALEDONIAMAURITIUSPacific OceanIndian OceanJun 13, 12:00 AM UTCJun 14, 12:00 AM UTCJun 15, 12:00 AM UTCJun 16, 12:00 AM UTCJun 17, 12:00 AM UTCJun 18, 12:00 AM UTCJun 19, 12:00 AM UTCJun 20, 12:00 AM UTCJun 21, 12:00 AM UTCJun 22, 12:00 AM UTCJun 23, 12:00 AM UTCJun 24, 12:00 AM UTCJun 25, 12:00 AM UTCJun 26, 12:00 AM UTCPeak: Category 5JUN 12JUN 26

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 935 mb
09201009702001020mphmbJun 12Jun 16Jun 21Jun 26
Forward speed 10 mphCumulative ACE 13.88 10⁴ kt²
002017.54035mph10⁴ kt²Jun 12Jun 16Jun 21Jun 26
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure935 hPa

Jun 16, 1963 during the tropical stage

Recorded track duration13.75 days

Full archive record, including non-tropical stages if present

Approximate track distance5,020 mi

Along the recorded center positions

STORM HISTORY

Strengthening east of the Philippines

The first archived position lies near 12.7°N, 135.3°E on 12 June. Shirley initially moved west and then north, strengthening over the Philippine Sea. At 00:00 UTC on 16 June, its one-minute sustained winds reached 140 kt and its pressure fell to 935 hPa.

Through the East China Sea toward Korea

Shirley moved northwest through the Ryukyu region and into the East China Sea, weakening as it gained latitude. It then turned northeast toward the Korean Peninsula. A sampled center-over-land observation late on 19 June carries winds of 58 kt.

The tropical-stage observations end early on 20 June. Later positions continue northeast past Japan and toward the date line, with the full archive ending on 26 June.

Further reading

NOAA IBTrACS v04r01 historical track archive

QUICK ANSWERS

Shirley in brief

What was Typhoon Shirley's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jun 16, 1963, 12:00 AM UTC.

What category was Typhoon Shirley?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Jun 15, 1963, 09:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Shirley's lowest pressure?

935 mb, the minimum central pressure recorded during its tropical stage, on Jun 16, 1963, 12:00 AM UTC.

When did Typhoon Shirley occur?

The archived track runs from Jun 12, 1963, 06:00 AM UTC to Jun 26, 1963, 12:00 AM UTC, with the tropical stage from Jun 12, 1963, 06:00 AM UTC to Jun 20, 1963, 03:00 AM UTC.

Where did Typhoon Shirley form?

In the Western Pacific basin, in the 1963 season. Its first archived position is 12.7°N, 135.3°E on Jun 12, 1963, 06:00 AM UTC.

Did Typhoon Shirley make landfall?

The archive places its center over land at 1 recorded position; the strongest is 67 mph on Jun 19, 1963, 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