1970 Western Pacific typhoon season

Typhoon Joan 1970

Typhoon Joan, known as Sening in the Philippines, devastated parts of Luzon in October 1970. After crossing the island, it grew into a broad storm over the South China Sea and continued toward Hainan and southern China.

PEAK INTENSITYCategory 5
JOAN: complete recorded track, Oct 9, 1970–Oct 18, 1970Recorded track from Oct 9, 1970 to Oct 18, 1970. Colors show the recorded wind category. The highlighted position follows the replay controls.JAPANTAIWANOct 9, 12:00 AM UTCOct 10, 12:00 AM UTCOct 11, 12:00 AM UTCOct 12, 12:00 AM UTCOct 13, 12:00 AM UTCOct 14, 12:00 AM UTCOct 15, 12:00 AM UTCOct 16, 12:00 AM UTCOct 17, 12:00 AM UTCOct 18, 12:00 AM UTCPeak: Category 5OCT 9OCT 18

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 173 mphPressure 910 mb
09001009602001020mphmbOct 9Oct 12Oct 15Oct 18
Forward speed 14 mphCumulative ACE 11.80 10⁴ kt²
0015153030mph10⁴ kt²Oct 9Oct 12Oct 15Oct 18
Maximum sustained wind173 mph

173 mph

Minimum recorded pressure905 hPa

Oct 12, 1970 during the tropical stage

Recorded track duration9.75 days

Full archive record, including non-tropical stages if present

Approximate track distance2,990 mi

Along the recorded center positions

STORM HISTORY

A destructive Bicol landfall

Joan developed near the Caroline Islands and strengthened while moving west. Its course turned northwest toward the Bicol Peninsula, and the archive records peak one-minute winds of 150 kt early on 13 October. It brushed Catanduanes before making landfall in the Lagonoy Gulf region that day.

Naga City suffered a direct hit. Flying debris, collapsing houses, fallen trees and flooding killed residents across the affected area. Joan continued over Luzon and passed just south of Manila on 14 October as a much weaker typhoon.

A broad storm over the South China Sea

Joan's core became less organized after the Luzon crossing, but its wind field expanded. Gale-force winds extended about 400 km from the center, disrupting shipping across much of the northern South China Sea. The storm turned north toward Hainan and made landfall on the Leizhou Peninsula before weakening over China.

Heavy losses before another typhoon

Joan left more than 80,000 people homeless in the Philippines and caused an estimated US$74 million in damage at 1970 values. The reported death toll reached 768 after 193 missing people were declared dead. Typhoon Kate struck later the same week, worsening conditions during the recovery.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Joan (1970)

QUICK ANSWERS

Joan in brief

What was Typhoon Joan's highest wind speed?

173 mph, the highest one-minute sustained wind in its tropical stage, recorded on Oct 13, 1970, 12:00 AM UTC.

What category was Typhoon Joan?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Oct 12, 1970, 06:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Joan's lowest pressure?

905 mb, the minimum central pressure recorded during its tropical stage, on Oct 12, 1970, 06:00 PM UTC.

When did Typhoon Joan occur?

The archived track runs from Oct 9, 1970, 12:00 AM UTC to Oct 18, 1970, 06:00 PM UTC, with the tropical stage from Oct 9, 1970, 12:00 PM UTC to Oct 18, 1970, 03:00 AM UTC.

Where did Typhoon Joan form?

In the Western Pacific basin, in the 1970 season. Its first archived position is 7.6°N, 147°E on Oct 9, 1970, 12:00 AM UTC.

Did Typhoon Joan make landfall?

The archive places its center over land at 4 recorded positions; the strongest is 132 mph on Oct 13, 1970, 06:00 AM 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