1999 Western Pacific typhoon season

Typhoon Bart 1999

Typhoon Bart crossed Japan in September 1999 after reaching Category 5 strength near Okinawa. Floods, landslides and strong winds damaged communities from the Ryukyu Islands to the main Japanese islands.

PEAK INTENSITYCategory 5
Satellite image of Bart 1999
National Oceanic and Atmospheric Administration (NOAA) and NASA Worldview, data processed by CooperScience and superimposed by Xyklone. public domain Source
Bart 1999: BART infrared satellite image, 1999-09-22T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
BART: complete recorded track, Sep 17, 1999–Sep 29, 1999Recorded track from Sep 17, 1999 to Sep 29, 1999. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAPHILIPPINESINDIAFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanSep 17, 12:00 AM UTCSep 18, 12:00 AM UTCSep 19, 12:00 AM UTCSep 20, 12:00 AM UTCSep 21, 12:00 AM UTCSep 22, 12:00 AM UTCSep 23, 12:00 AM UTCSep 24, 12:00 AM UTCSep 25, 12:00 AM UTCSep 26, 12:00 AM UTCSep 27, 12:00 AM UTCSep 28, 12:00 AM UTCSep 29, 12:00 AM UTCPeak: Category 5SEP 17SEP 29

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 935 mb
09201009702001020mphmbSep 17Sep 21Sep 25Sep 29
Forward speed 5 mphCumulative ACE 12.28 10⁴ kt²
002512.55025mph10⁴ kt²Sep 17Sep 21Sep 25Sep 29
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure930 hPa

Sep 22, 1999 during the tropical stage

Recorded track duration12.25 days

Full archive record, including non-tropical stages if present

Approximate track distance4,280 mi

Along the recorded center positions

STORM HISTORY

Strengthening near Okinawa

Bart developed south of Okinawa within the monsoon trough. Its early growth was slow, but conditions improved as upper-level winds changed. It became a typhoon on September 20, paused southwest of Okinawa and then moved north. Peak one-minute winds reached 140 kt on September 22, with a minimum central pressure of 930 hPa.

Bart passed about 75 kilometers west of Okinawa before weakening. It accelerated northeast, made landfall near Omuta on Kyushu and crossed Honshu. The storm then entered the Sea of Japan and continued toward the North Pacific as an extratropical system.

Flooding and widespread disruption

Rainfall reached 1,180 millimeters at Funato in Kochi Prefecture. Flooding, more than 245 landslides and fallen trees damaged buildings and transport routes. Officials canceled flights and ferries, disrupted train services and closed schools across affected areas.

The saved account records 36 deaths and more than 1,300 injuries. Floodwater entered 18,498 homes, and about 813,000 households lost electricity. Kumamoto Prefecture suffered some of the worst damage during Bart's passage across Kyushu.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Bart (1999)

QUICK ANSWERS

Bart in brief

What was Typhoon Bart's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Sep 22, 1999, 06:00 AM UTC.

What category was Typhoon Bart?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Sep 22, 1999, 06:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Bart's lowest pressure?

930 mb, the minimum central pressure recorded during its tropical stage, on Sep 22, 1999, 12:00 PM UTC.

When did Typhoon Bart occur?

The archived track runs from Sep 17, 1999, 12:00 AM UTC to Sep 29, 1999, 06:00 AM UTC, with the tropical stage from Sep 17, 1999, 12:00 AM UTC to Sep 25, 1999, 12:00 AM UTC.

Where did Typhoon Bart form?

In the Western Pacific basin, in the 1999 season. Its first archived position is 20.4°N, 129.7°E on Sep 17, 1999, 12:00 AM UTC.

Did Typhoon Bart make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 109 mph on Sep 23, 1999, 09:00 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