1966 Western Pacific typhoon season

Typhoon Kit 1966

Typhoon Kit stayed offshore as it passed Japan in June 1966, yet its rain caused widespread flooding and landslides. The storm disrupted railways and Tokyo's subway system after an exceptionally intense phase over the Philippine Sea.

PEAK INTENSITYCategory 5
KIT: complete recorded track, Jun 20, 1966–Jul 3, 1966Recorded track from Jun 20, 1966 to Jul 3, 1966. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAASIAINDIATAIWANFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanJun 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 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 UTCPeak: Category 5JUN 20JUL 3

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 196 mphPressure 910 mb
08801009502001020mphmbJun 20Jun 24Jun 29Jul 3
Forward speed 16 mphCumulative ACE 10.68 10⁴ kt²
0020154030mph10⁴ kt²Jun 20Jun 24Jun 29Jul 3
Maximum sustained wind196 mph

196 mph

Minimum recorded pressure880 hPa

Jun 26, 1966 during the tropical stage

Recorded track duration13.75 days

Full archive record, including non-tropical stages if present

Approximate track distance5,620 mi

Along the recorded center positions

STORM HISTORY

A contracting eye and falling pressure

Kit developed near Chuuk and moved west before turning northwest. It became a typhoon late on 23 June. During rapid intensification on 24 and 25 June, its eye contracted and its central pressure fell sharply.

The archive records peak one-minute winds of 170 kt and a minimum pressure of 880 hPa on 26 June. Kit then weakened while accelerating north-northeast. On 28 June, it passed about 155 km east of Tokyo, retaining typhoon strength without making a recorded landfall.

Flooding across eastern Japan

Torrential rain flooded more than 128,000 homes in Japan, with 433 reported collapsed. Landslides blocked or destroyed roads, while the Tokyo–Osaka railway was interrupted for 12 hours. Floodwater also shut down Tokyo's subway system, stranding large numbers of commuters.

Japan reported 64 deaths and 19 people missing. A separate accident during recovery killed 25 workers repairing an irrigation tunnel near Utsunomiya: exhaust from a portable generator caused carbon monoxide poisoning.

Kit became extratropical south of Hokkaido on 29 June. Its archived continuation heads east across the northern Pacific and ends near the International Date Line on 3 July.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 1966 Pacific typhoon season, Kit section

QUICK ANSWERS

Kit in brief

What was Typhoon Kit's highest wind speed?

196 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jun 26, 1966, 12:00 AM 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 25, 1966, 06:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Kit's lowest pressure?

880 mb, the minimum central pressure recorded during its tropical stage, on Jun 26, 1966, 06:00 AM UTC.

When did Typhoon Kit occur?

The archived track runs from Jun 20, 1966, 12:00 AM UTC to Jul 3, 1966, 06:00 PM UTC, with the tropical stage from Jun 20, 1966, 06:00 AM UTC to Jun 29, 1966, 03:00 AM UTC.

Where did Typhoon Kit form?

In the Western Pacific basin, in the 1966 season. Its first archived position is 8.7°N, 150.8°E on Jun 20, 1966, 12:00 AM UTC.

Did Typhoon Kit make landfall?

No archived position places Typhoon Kit'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