1957 Western Pacific typhoon season

Typhoon Virginia 1957

Typhoon Virginia passed near the Philippines and struck Taiwan in June 1957 before continuing toward Japan. It reached Category 5 strength east of Luzon, then weakened during its northward journey. Flooding and wind damaged homes and ships along the storm's later path.

PEAK INTENSITYCategory 5
VIRGINIA: complete recorded track, Jun 17, 1957–Jun 28, 1957Recorded track from Jun 17, 1957 to Jun 28, 1957. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAFIJITONGAVANUATUNEW CALEDONIAIndian OceanJun 18, 12:00 AM UTCJun 19, 12:00 AM UTCJun 20, 12:00 AM UTCJun 21, 12:00 AM UTCJun 22, 12:00 AM UTCJun 23, 12:00 AM UTCJun 24, 12:00 AM UTCJun 25, 12:00 AM UTCJun 26, 12:00 AM UTCJun 27, 12:00 AM UTCJun 28, 12:00 AM UTCPeak: Category 5JUN 17JUN 28

Drag to pan. Pinch or Ctrl/⌘ + scroll to zoom. Keyboard: plus or minus to zoom, arrow keys to pan, and 0 to show the full track.

DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 173 mphPressure 900 mb
09001009602001020mphmbJun 17Jun 21Jun 24Jun 28
Forward speed 12 mphCumulative ACE 13.94 10⁴ kt²
0025205040mph10⁴ kt²Jun 17Jun 21Jun 24Jun 28
Maximum sustained wind173 mph

173 mph

Minimum recorded pressure900 hPa

Jun 22, 1957 during the tropical stage

Recorded track duration11.25 days

Full archive record, including non-tropical stages if present

Approximate track distance4,210 mi

Along the recorded center positions

STORM HISTORY

Intensification east of Luzon

Virginia developed over the western Pacific in mid-June and moved northwest. It strengthened into a tropical storm on 19 June and intensified further over the following days. The archive records peak one-minute winds of 150 kt and a pressure of 900 hPa at 06:00 UTC on 22 June.

Taiwan and southern Japan

Virginia passed near the Philippines before making landfall in Taiwan. It then moved toward the waters between Korea and Japan. The strongest sampled center-over-land observation carries winds of 90 kt on 25 June, below its earlier Category 5 peak.

The historical account reports 30 deaths, 23 missing people and 33 injuries in the Japanese disaster record, along with 396 houses and fourteen ships destroyed. Floods affected about 150,000 people in southern Japan. Taiwan also suffered deaths and damage, and its government allocated 100,000 New Taiwan dollars for relief.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Virginia (1957)

QUICK ANSWERS

Virginia in brief

What was Typhoon Virginia's highest wind speed?

173 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jun 22, 1957, 06:00 AM UTC.

What category was Typhoon Virginia?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Jun 21, 1957, 06:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Virginia's lowest pressure?

900 mb, the minimum central pressure recorded during its tropical stage, on Jun 22, 1957, 06:00 AM UTC.

When did Typhoon Virginia occur?

The archived track runs from Jun 17, 1957, 06:00 AM UTC to Jun 28, 1957, 12:00 PM UTC, with the tropical stage from Jun 18, 1957, 06:00 AM UTC to Jun 28, 1957, 12:00 PM UTC.

Where did Typhoon Virginia form?

In the Western Pacific basin, in the 1957 season. Its first archived position is 5.4°N, 155.5°E on Jun 17, 1957, 06:00 AM UTC.

Did Typhoon Virginia make landfall?

The archive places its center over land at 1 recorded position; the strongest is 104 mph on Jun 25, 1957, 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