1967 Western Pacific typhoon season

Typhoon Emma 1967

Typhoon Emma, known as Welming in the Philippines, crossed southern Luzon in November 1967. The storm destroyed homes, damaged shipping and left a large population homeless before continuing toward southern China.

PEAK INTENSITYCategory 5
EMMA: complete recorded track, Oct 30, 1967–Nov 8, 1967Recorded track from Oct 30, 1967 to Nov 8, 1967. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANTAIWANOct 30, 12:00 AM UTCOct 31, 12:00 AM UTCNov 1, 12:00 AM UTCNov 2, 12:00 AM UTCNov 3, 12:00 AM UTCNov 4, 12:00 AM UTCNov 5, 12:00 AM UTCNov 6, 12:00 AM UTCNov 7, 12:00 AM UTCNov 8, 12:00 AM UTCPeak: Category 5OCT 30NOV 8

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 930 mb
09001009602001020mphmbOct 30Nov 2Nov 5Nov 8
Forward speed 17 mphCumulative ACE 10.64 10⁴ kt²
001512.53025mph10⁴ kt²Oct 30Nov 2Nov 5Nov 8
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure908 hPa

Nov 3, 1967 during the tropical stage

Recorded track duration9.75 days

Full archive record, including non-tropical stages if present

Approximate track distance3,070 mi

Along the recorded center positions

STORM HISTORY

Strengthening between Micronesia and Luzon

Emma developed on 30 October and became a typhoon the following day. It traveled west-northwest, passing south of Yap before intensifying rapidly over the Philippine Sea. Peak archived one-minute winds reached 140 kt on 2 November.

The typhoon reached southern Luzon on 3 November after weakening from its offshore peak. The island's mountainous terrain reduced Emma's strength further, and it emerged over the South China Sea as a tropical storm.

Destruction in the Philippines

More than 300 deaths were reported in the Philippines, where over 140,000 people were left homeless. Two ships sank and others were damaged. Philippine damage was estimated at US$75.6 million in 1967 values, while Yap and Palau also suffered property losses.

Emma continued across the South China Sea and made its final landfall near Zhanjiang as a tropical storm. It dissipated on 8 November near the border region between China and Vietnam, ending a route that had stretched westward from Micronesia.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Emma (1967)

QUICK ANSWERS

Emma in brief

What was Typhoon Emma's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Nov 2, 1967, 12:00 PM UTC.

What category was Typhoon Emma?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Nov 2, 1967, 09:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Emma's lowest pressure?

908 mb, the minimum central pressure recorded during its tropical stage, on Nov 3, 1967, 12:00 AM UTC.

When did Typhoon Emma occur?

The archived track runs from Oct 30, 1967, 12:00 AM UTC to Nov 8, 1967, 06:00 PM UTC, with the tropical stage from Oct 30, 1967, 06:00 AM UTC to Nov 8, 1967, 06:00 PM UTC.

Where did Typhoon Emma form?

In the Western Pacific basin, in the 1967 season. Its first archived position is 6.5°N, 150°E on Oct 30, 1967, 12:00 AM UTC.

Did Typhoon Emma make landfall?

The archive places its center over land at 4 recorded positions; the strongest is 119 mph on Nov 3, 1967, 03:00 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