1970 Western Pacific typhoon season

Typhoon Olga 1970

Typhoon Olga reached exceptional intensity over the Philippine Sea before weakening on its approach to Japan in July 1970. Heavy rain caused deadly flooding and landslides even after the storm's winds had fallen far below their offshore peak.

PEAK INTENSITYCategory 5
OLGA: complete recorded track, Jun 26, 1970–Jul 7, 1970Recorded track from Jun 26, 1970 to Jul 7, 1970. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAPHILIPPINESFIJITONGAVANUATUNEW CALEDONIAJun 27, 12:00 AM UTCJun 28, 12:00 AM UTCJun 29, 12:00 AM UTCJun 30, 12:00 AM UTCJul 1, 12:00 AM UTCJul 2, 12:00 AM UTCJul 3, 12:00 AM UTCJul 4, 12:00 AM UTCJul 5, 12:00 AM UTCJul 6, 12:00 AM UTCJul 7, 12:00 AM UTCPeak: Category 5JUN 26JUL 7

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 905 mb
09001009602001020mphmbJun 26Jun 30Jul 3Jul 7
Forward speed 13 mphCumulative ACE 10.37 10⁴ kt²
0015153030mph10⁴ kt²Jun 26Jun 30Jul 3Jul 7
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure905 hPa

Jul 1, 1970 during the tropical stage

Recorded track duration10.75 days

Full archive record, including non-tropical stages if present

Approximate track distance4,130 mi

Along the recorded center positions

STORM HISTORY

Rapid development in the Philippine Sea

Olga began as a tropical wave near the Marshall Islands. Strong easterly winds carried it west through the Caroline Islands, and a closed circulation organized south of Guam. As steering winds weakened, Olga slowed, turned northwest and intensified rapidly.

The archive records peak one-minute winds of 140 kt on 1 July. Olga then moved north through a break in the subtropical ridge. It weakened east of Taiwan as drier air entered the circulation and its track bent toward Japan.

Rain in Japan and South Korea

Olga reached Japan's Kansai region south of Osaka on 5 July as a tropical storm. Rainfall reached about 14 inches in some places, producing landslides and extensive flooding. Twenty deaths were reported in Japan.

After entering the Sea of Japan, the circulation merged with a cold front. Heavy rainfall associated with Olga's remnants also affected South Korea, where 29 deaths were reported. The archived track continues through 7 July.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 1970 Pacific typhoon season, Olga section

QUICK ANSWERS

Olga in brief

What was Typhoon Olga's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jul 1, 1970, 12:00 PM UTC.

What category was Typhoon Olga?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Jul 1, 1970, 09:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Olga's lowest pressure?

905 mb, the minimum central pressure recorded during its tropical stage, on Jul 1, 1970, 06:00 AM UTC.

When did Typhoon Olga occur?

The archived track runs from Jun 26, 1970, 12:00 PM UTC to Jul 7, 1970, 06:00 AM UTC, with the tropical stage from Jun 28, 1970, 06:00 AM UTC to Jul 5, 1970, 09:00 PM UTC.

Where did Typhoon Olga form?

In the Western Pacific basin, in the 1970 season. Its first archived position is 7°N, 153.4°E on Jun 26, 1970, 12:00 PM UTC.

Did Typhoon Olga make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 58 mph on Jul 5, 1970, 12:00 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