1962 Western Pacific typhoon season

Typhoon Karen 1962

Typhoon Karen devastated Guam in November 1962, damaging or destroying almost all of the island's homes. The storm crippled utilities and communications and left tens of thousands without shelter. Recovery brought a major relief operation and changes to building standards.

PEAK INTENSITYCategory 5
Image of Karen 1962
United States Weather Bureau. public domain Source
KAREN: complete recorded track, Nov 7, 1962–Nov 18, 1962Recorded track from Nov 7, 1962 to Nov 18, 1962. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANPHILIPPINESTAIWANFIJITONGAVANUATUNEW CALEDONIAPacific OceanNov 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 7NOV 18

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 184 mphPressure 920 mb
09001009602001020mphmbNov 7Nov 11Nov 14Nov 18
Forward speed 6 mphCumulative ACE 6.43 10⁴ kt²
0040358070mph10⁴ kt²Nov 7Nov 11Nov 14Nov 18
Maximum sustained wind184 mph

184 mph

Minimum recorded pressure900 hPa

Nov 13, 1962 during the tropical stage

Recorded track duration11.5 days

Full archive record, including non-tropical stages if present

Approximate track distance6,240 mi

Along the recorded center positions

STORM HISTORY

Rapid development before Guam

Karen developed southeast of Chuuk and intensified rapidly while moving north. It became a Category 5 equivalent by 9 November, then turned west toward Guam. The archive first records its maximum one-minute wind estimate of 160 kt at 00:00 UTC on 9 November.

Karen struck Guam on 11 November while still an exceptionally intense typhoon. It later strengthened again west of the island before turning north and northeast. The site's minimum archived pressure of 900 hPa occurs on 13 November.

An island without shelter and utilities

About 95 percent of Guam's homes suffered damage or destruction, leaving at least 45,000 people homeless. Authorities established water-distribution centers after utilities failed. The reported island losses reached US$250 million in 1962 dollars, with eleven deaths.

Evacuation and rebuilding

Relief crews evacuated thousands to California, Hawaii and Wake Island. Others stayed in public buildings and tent settlements for months. More than US$60 million in relief funding supported recovery over the following years, and rebuilding introduced stronger construction standards.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Karen

QUICK ANSWERS

Karen in brief

What was Typhoon Karen's highest wind speed?

184 mph, the highest one-minute sustained wind in its tropical stage, recorded on Nov 9, 1962, 12:00 AM UTC.

What category was Typhoon Karen?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Nov 8, 1962, 09:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Karen's lowest pressure?

900 mb, the minimum central pressure recorded during its tropical stage, on Nov 13, 1962, 12:00 AM UTC.

When did Typhoon Karen occur?

The archived track runs from Nov 7, 1962, 06:00 AM UTC to Nov 18, 1962, 06:00 PM UTC, with the tropical stage from Nov 7, 1962, 06:00 AM UTC to Nov 18, 1962, 06:00 PM UTC.

Where did Typhoon Karen form?

In the Western Pacific basin, in the 1962 season. Its first archived position is 6°N, 154°E on Nov 7, 1962, 06:00 AM UTC.

Did Typhoon Karen make landfall?

No archived position places Typhoon Karen'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