1952 Western Pacific typhoon season

Typhoon Wilma 1952

Typhoon Wilma crossed the western Pacific in October 1952, reaching Category 5 strength before passing through the Philippines. It continued across the South China Sea and reached Vietnam as a tropical storm, completing a westward journey from Micronesian waters to mainland Southeast Asia.

PEAK INTENSITYCategory 5
WILMA: complete recorded track, Oct 21, 1952–Oct 31, 1952Recorded track from Oct 21, 1952 to Oct 31, 1952. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANTAIWANVANUATUNEW CALEDONIAOct 22, 12:00 AM UTCOct 23, 12:00 AM UTCOct 24, 12:00 AM UTCOct 25, 12:00 AM UTCOct 26, 12:00 AM UTCOct 27, 12:00 AM UTCOct 28, 12:00 AM UTCOct 29, 12:00 AM UTCOct 30, 12:00 AM UTCOct 31, 12:00 AM UTCPeak: Category 5OCT 21OCT 31

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 184 mphPressure 930 mb
09201009702001020mphmbOct 21Oct 24Oct 28Oct 31
Forward speed 20 mphCumulative ACE 16.39 10⁴ kt²
0015203040mph10⁴ kt²Oct 21Oct 24Oct 28Oct 31
Maximum sustained wind184 mph

184 mph

Minimum recorded pressure930 hPa

Oct 25, 1952 during the tropical stage

Recorded track duration10 days

Full archive record, including non-tropical stages if present

Approximate track distance3,510 mi

Along the recorded center positions

STORM HISTORY

Strengthening toward the Philippines

The archive begins Wilma's track on 21 October near 5.5°N, 152°E. Over the following days, the storm traveled west toward the Philippines and intensified. US-agency estimates first reached Category 5 strength at 12:00 UTC on 25 October, then peaked at 160 kt at 00:00 UTC on 26 October.

Through the Philippines and across the South China Sea

Wilma weakened before crossing the Philippines. At 21:00 UTC on 27 October, the sampled archive places its center over land near 12.4°N, 121.3°E, with sustained winds of 80 kt. That observation describes a much weaker cyclone than the Category 5 storm recorded east of the islands.

After emerging into the South China Sea, Wilma continued toward Vietnam. It made landfall there as a tropical storm and dissipated on 31 October. The archived track spans ten days, following the cyclone from the western Pacific across the Philippine archipelago to the Asian mainland.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 1952 Pacific typhoon season, Wilma section

QUICK ANSWERS

Wilma in brief

What was Typhoon Wilma's highest wind speed?

184 mph, the highest one-minute sustained wind in its tropical stage, recorded on Oct 26, 1952, 12:00 AM UTC.

What category was Typhoon Wilma?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Oct 25, 1952, 12:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Wilma's lowest pressure?

930 mb, the minimum central pressure recorded during its tropical stage, on Oct 25, 1952, 06:00 PM UTC.

When did Typhoon Wilma occur?

The archived track runs from Oct 21, 1952, 12:00 PM UTC to Oct 31, 1952, 12:00 PM UTC, with the tropical stage from Oct 21, 1952, 12:00 PM UTC to Oct 31, 1952, 12:00 PM UTC.

Where did Typhoon Wilma form?

In the Western Pacific basin, in the 1952 season. Its first archived position is 5.5°N, 152°E on Oct 21, 1952, 12:00 PM UTC.

Did Typhoon Wilma make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 92 mph on Oct 27, 1952, 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