1996 Western Pacific typhoon season

Typhoon Eve 1996

Typhoon Eve reached southern Japan in July 1996 after a short, intense phase over the western Pacific. It weakened over mountainous terrain, then regained tropical-storm strength east of the country.

PEAK INTENSITYCategory 5
Eve 1996: EVE infrared satellite image, 1996-07-16T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
EVE: complete recorded track, Jul 10, 1996–Jul 27, 1996Recorded track from Jul 10, 1996 to Jul 27, 1996. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAPHILIPPINESINDIATAIWANFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanJul 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 UTCPeak: Category 5JUL 10JUL 27

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 945 mb
09401009802001020mphmbJul 10Jul 16Jul 21Jul 27
Forward speed 10 mphCumulative ACE 8.27 10⁴ kt²
001512.53025mph10⁴ kt²Jul 10Jul 16Jul 21Jul 27
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure940 hPa

Jul 16, 1996 during the tropical stage

Recorded track duration17.5 days

Full archive record, including non-tropical stages if present

Approximate track distance5,520 mi

Along the recorded center positions

STORM HISTORY

A rapid rise in strength

Eve developed over the open western Pacific and moved west-northwest. It became a tropical storm on July 14 and a typhoon the following day. The archive records maximum one-minute winds of 140 kt on July 16, equivalent to Category 5, and a minimum central pressure of 940 hPa.

Changes in the eyewall interrupted Eve's strongest phase before it reached southern Japan on July 18. The typhoon weakened over the mountains and turned east across the islands. Its archived overland positions reflect a weaker storm than the Category 5 system observed offshore two days earlier.

Across Japan and back to sea

The saved season account reports nine injuries and no deaths in Japan. After leaving the islands, Eve regained tropical-storm strength over the ocean and continued northeast. The archive follows the system through July 27, several days beyond the end of its tropical phase.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 1996 Pacific typhoon season, Eve section

QUICK ANSWERS

Eve in brief

What was Typhoon Eve's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Jul 16, 1996, 12:00 AM UTC.

What category was Typhoon Eve?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Jul 15, 1996, 09:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Eve's lowest pressure?

940 mb, the minimum central pressure recorded during its tropical stage, on Jul 16, 1996, 03:00 AM UTC.

When did Typhoon Eve occur?

The archived track runs from Jul 10, 1996, 06:00 AM UTC to Jul 27, 1996, 06:00 PM UTC, with the tropical stage from Jul 13, 1996, 06:00 AM UTC to Jul 24, 1996, 09:00 AM UTC.

Where did Typhoon Eve form?

In the Western Pacific basin, in the 1996 season. Its first archived position is 19.3°N, 151.5°E on Jul 10, 1996, 06:00 AM UTC.

Did Typhoon Eve make landfall?

The archive places its center over land at 4 recorded positions; the strongest is 90 mph on Jul 18, 1996, 09:00 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