1953 Western Pacific typhoon season

Typhoon Kit 1953

Typhoon Kit followed a long route across East Asia in June and July 1953. After reaching Category 5 strength over the western Pacific, it weakened on its approach to Taiwan and continued toward China, Korea and Japan. Strong winds and rain also affected the northern Philippines.

PEAK INTENSITYCategory 5
KIT: complete recorded track, Jun 25, 1953–Jul 8, 1953Recorded track from Jun 25, 1953 to Jul 8, 1953. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAASIAJAPANINDIAFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanJun 25, 12:00 AM UTCJun 26, 12:00 AM UTCJun 27, 12:00 AM UTCJun 28, 12:00 AM UTCJun 29, 12:00 AM UTCJun 30, 12:00 AM UTCJul 1, 12:00 AM UTCJul 2, 12:00 AM UTCJul 3, 12:00 AM UTCJul 4, 12:00 AM UTCJul 5, 12:00 AM UTCJul 6, 12:00 AM UTCJul 7, 12:00 AM UTCJul 8, 12:00 AM UTCPeak: Category 5JUN 25JUL 8

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 173 mphPressure 920 mb
09001009602001020mphmbJun 25Jun 29Jul 3Jul 8
Forward speed 16 mphCumulative ACE 12.70 10⁴ kt²
002022.54045mph10⁴ kt²Jun 25Jun 29Jul 3Jul 8
Maximum sustained wind173 mph

173 mph

Minimum recorded pressure910 hPa

Jun 30, 1953 during the tropical stage

Recorded track duration13.25 days

Full archive record, including non-tropical stages if present

Approximate track distance4,450 mi

Along the recorded center positions

STORM HISTORY

A June peak over the Pacific

Kit's archived track begins on 25 June near 5°N, 150°E, east of the Philippines. It traveled west and then northwest, reaching one-minute sustained winds of 150 kt at 12:00 UTC on 29 June. The minimum archived pressure of 910 hPa followed at 00:00 UTC on 30 June.

Taiwan and the northward turn

Kit slowed as July began and reached Taiwan on 3 July. It then moved into China and turned north, continuing toward the Korean Peninsula and Japan. The historical account places its later passage across Japan on 7 July; the archive ends on 8 July.

The storm brought strong winds and widespread rain to Batanes in the northern Philippines. Maritime losses included one ship destroyed and another damaged. By the time Kit reached land, it had weakened from its oceanic peak: the strongest sampled center-over-land observation carries 90 kt on 3 July.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 1953 Pacific typhoon season, Kit section

QUICK ANSWERS

Kit in brief

What was Typhoon Kit's highest wind speed?

173 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jun 29, 1953, 12:00 PM UTC.

What category was Typhoon Kit?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Jun 29, 1953, 12:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Kit's lowest pressure?

910 mb, the minimum central pressure recorded during its tropical stage, on Jun 30, 1953, 12:00 AM UTC.

When did Typhoon Kit occur?

The archived track runs from Jun 25, 1953, 12:00 AM UTC to Jul 8, 1953, 06:00 AM UTC, with the tropical stage from Jun 25, 1953, 12:00 AM UTC to Jul 8, 1953, 06:00 AM UTC.

Where did Typhoon Kit form?

In the Western Pacific basin, in the 1953 season. Its first archived position is 5°N, 150°E on Jun 25, 1953, 12:00 AM UTC.

Did Typhoon Kit make landfall?

The archive places its center over land at 3 recorded positions; the strongest is 104 mph on Jul 3, 1953, 06:00 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