1972 Western Pacific typhoon season

Typhoon Rita 1972

Typhoon Rita spent much of July 1972 wandering across the western Pacific and East China Sea. Interactions with other typhoons repeatedly changed its course, producing an unusually long history of stalls, loops and renewed strengthening.

PEAK INTENSITYCategory 5
Image of Rita 1972
Joint Typhoon Warning Center. public domain Source
RITA: complete recorded track, Jul 5, 1972–Jul 30, 1972Recorded track from Jul 5, 1972 to Jul 30, 1972. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAJAPANPHILIPPINESINDIAFIJITONGAVANUATUNEW CALEDONIAMAURITIUSPacific OceanIndian OceanJul 5, 12:00 AM UTCJul 6, 12:00 AM UTCJul 7, 12:00 AM UTCJul 8, 12:00 AM UTCJul 9, 12:00 AM UTCJul 10, 12:00 AM UTCJul 11, 12:00 AM UTCJul 12, 12:00 AM UTCJul 13, 12:00 AM UTCJul 14, 12:00 AM UTCJul 15, 12:00 AM UTCJul 16, 12:00 AM UTCJul 17, 12:00 AM UTCJul 18, 12:00 AM UTCJul 19, 12:00 AM UTCJul 20, 12:00 AM UTCJul 21, 12:00 AM UTCJul 22, 12:00 AM UTCJul 23, 12:00 AM UTCJul 24, 12:00 AM UTCJul 25, 12:00 AM UTCJul 26, 12:00 AM UTCJul 27, 12:00 AM UTCJul 28, 12:00 AM UTCJul 29, 12:00 AM UTCJul 30, 12:00 AM UTCPeak: Category 5JUL 5JUL 30

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 167 mphPressure 910 mb
09001009602001020mphmbJul 5Jul 13Jul 21Jul 30
Forward speed 6 mphCumulative ACE 17.45 10⁴ kt²
002032.54065mph10⁴ kt²Jul 5Jul 13Jul 21Jul 30
Maximum sustained wind167 mph

167 mph

Minimum recorded pressure910 hPa

Jul 11, 1972 during the tropical stage

Recorded track duration25 days

Full archive record, including non-tropical stages if present

Approximate track distance5,360 mi

Along the recorded center positions

STORM HISTORY

A powerful peak followed by changing tracks

Rita developed southeast of Guam and strengthened while moving west and northwest. The archive records peak one-minute winds of 145 kt on 11 July. It then weakened sharply as the upper-level airflow that had supported its development changed.

Nearby Typhoon Phyllis influenced Rita's motion, slowing it and helping turn it northeast. The two circulations interacted through the Fujiwhara effect, in which nearby cyclones rotate around a shared center. Rita stalled again as Phyllis moved toward Japan.

A broad circulation and a Ryukyu loop

Rita regained some strength and expanded dramatically. By 18 July, gale-force winds covered an area roughly 1,290 km across. It passed through the Ryukyus near Amami Oshima on 20 July, then turned southwest over the East China Sea under the influence of another nearby typhoon, Tess.

A loop carried Rita back near Miyako-jima and Okinawa before it accelerated north toward Jeju and the Yellow Sea. The weakening system subsequently reached northern China, with remnants persisting through 30 July. The saved historical account attributes 377 direct and indirect deaths to Rita's effects across several countries, including flood and disease deaths in the Philippines.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Rita (1972)

QUICK ANSWERS

Rita in brief

What was Typhoon Rita's highest wind speed?

167 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jul 11, 1972, 12:00 AM UTC.

What category was Typhoon Rita?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Jul 10, 1972, 09:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Rita's lowest pressure?

910 mb, the minimum central pressure recorded during its tropical stage, on Jul 11, 1972, 12:00 AM UTC.

When did Typhoon Rita occur?

The archived track runs from Jul 5, 1972, 12:00 AM UTC to Jul 30, 1972, 12:00 AM UTC, with the tropical stage from Jul 6, 1972, 12:00 PM UTC to Jul 26, 1972, 09:00 AM UTC.

Where did Typhoon Rita form?

In the Western Pacific basin, in the 1972 season. Its first archived position is 9.5°N, 150.5°E on Jul 5, 1972, 12:00 AM UTC.

Did Typhoon Rita make landfall?

No archived position places Typhoon Rita'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