1957 Western Pacific typhoon season

Typhoon Kit 1957

Typhoon Kit struck northern Luzon during the Philippine election in November 1957. Wind and torrential rain damaged polling places, homes and other property, disrupting voting across a large part of the country. The storm had reached Category 5 strength before approaching the islands.

PEAK INTENSITYCategory 5
KIT: complete recorded track, Nov 4, 1957–Nov 18, 1957Recorded track from Nov 4, 1957 to Nov 18, 1957. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANNov 5, 12:00 AM UTCNov 6, 12:00 AM UTCNov 7, 12:00 AM UTCNov 8, 12:00 AM UTCNov 9, 12:00 AM UTCNov 10, 12:00 AM UTCNov 11, 12:00 AM UTCNov 12, 12:00 AM UTCNov 13, 12:00 AM UTCNov 14, 12:00 AM UTCNov 15, 12:00 AM UTCNov 16, 12:00 AM UTCNov 17, 12:00 AM UTCNov 18, 12:00 AM UTCPeak: Category 5NOV 4NOV 18

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 915 mb
09001009602001020mphmbNov 4Nov 9Nov 13Nov 18
Forward speed 16 mphCumulative ACE 11.24 10⁴ kt²
0025155030mph10⁴ kt²Nov 4Nov 9Nov 13Nov 18
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure910 hPa

Nov 11, 1957 during the tropical stage

Recorded track duration13.25 days

Full archive record, including non-tropical stages if present

Approximate track distance4,750 mi

Along the recorded center positions

STORM HISTORY

Intensification toward Luzon

Kit developed over the western Pacific and moved west, intensifying faster after reaching tropical-storm strength. Its archived one-minute winds peaked at 140 kt at 12:00 UTC on 10 November. The minimum pressure of 910 hPa followed on 11 November, as Kit approached the northern Philippines.

An election interrupted

Kit crossed northern Luzon on 11 November. Torrential rain and high winds affected nearly half of the 7.2 million people expected to vote, and some polling places washed away. At least nineteen people died in the Philippines, and thousands lost their homes.

The strongest sampled center-over-land observation carries winds of 105 kt, after the storm had weakened from its peak. Kit regained some strength after leaving the islands, then continued toward the Ryukyu region. Its tropical-stage observations end on 16 November, with the full track extending through 18 November.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 1957 Pacific typhoon season, Kit section

QUICK ANSWERS

Kit in brief

What was Typhoon Kit's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Nov 10, 1957, 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 Nov 10, 1957, 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 Nov 11, 1957, 06:00 AM UTC.

When did Typhoon Kit occur?

The archived track runs from Nov 4, 1957, 06:00 PM UTC to Nov 18, 1957, 12:00 AM UTC, with the tropical stage from Nov 7, 1957, 12:00 AM UTC to Nov 16, 1957, 03:00 PM UTC.

Where did Typhoon Kit form?

In the Western Pacific basin, in the 1957 season. Its first archived position is 10.6°N, 160.6°E on Nov 4, 1957, 06:00 PM UTC.

Did Typhoon Kit make landfall?

The archive places its center over land at 1 recorded position; the strongest is 121 mph on Nov 11, 1957, 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