2000 Western Pacific typhoon season

Typhoon Saomai 2000

Typhoon Saomai contributed to severe flooding in Japan before reaching South Korea in September 2000. Its interaction with a weather front produced exceptional rain far from the storm's strongest winds.

PEAK INTENSITYCategory 5
Satellite image of Saomai 2000
NASA, LAADS Web, HDF File processed by Supportstorm. public domain Source
Saomai 2000: SAOMAI infrared satellite image, 2000-09-10T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
SAOMAI: complete recorded track, Aug 31, 2000–Sep 19, 2000Recorded track from Aug 31, 2000 to Sep 19, 2000. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANPHILIPPINESINDIAFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanSep 1, 12:00 AM UTCSep 2, 12:00 AM UTCSep 3, 12:00 AM UTCSep 4, 12:00 AM UTCSep 5, 12:00 AM UTCSep 6, 12:00 AM UTCSep 7, 12:00 AM UTCSep 8, 12:00 AM UTCSep 9, 12:00 AM UTCSep 10, 12:00 AM UTCSep 11, 12:00 AM UTCSep 12, 12:00 AM UTCSep 13, 12:00 AM UTCSep 14, 12:00 AM UTCSep 15, 12:00 AM UTCSep 16, 12:00 AM UTCSep 17, 12:00 AM UTCSep 18, 12:00 AM UTCSep 19, 12:00 AM UTCPeak: Category 5AUG 31SEP 19

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 925 mb
09201009702001020mphmbAug 31Sep 6Sep 12Sep 19
Forward speed 5 mphCumulative ACE 18.97 10⁴ kt²
0020204040mph10⁴ kt²Aug 31Sep 6Sep 12Sep 19
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure925 hPa

Sep 10, 2000 during the tropical stage

Recorded track duration18.25 days

Full archive record, including non-tropical stages if present

Approximate track distance4,730 mi

Along the recorded center positions

STORM HISTORY

Two periods of strengthening

Saomai developed over the western Pacific at the end of August and reached an initial typhoon peak on September 4. Wind shear then weakened it to a tropical storm. It regained typhoon strength on September 9 and intensified to maximum one-minute winds of 140 kt and a central pressure of 925 hPa the next day.

The storm passed Okinawa, entered the East China Sea and curved northeast toward South Korea. It reached the Korean coast as a severe tropical storm, then became extratropical on September 16. Its remnants continued into Russia.

Floods ahead of the center

Moisture associated with Saomai interacted with a front over Japan, producing record rainfall in Nagoya and widespread flooding. Officials evacuated about 400,000 people across three prefectures. The saved account attributes eleven deaths and ¥978 billion in damage across Japan and its outlying islands to the event, in 2000 currency.

In South Korea, eight people died, and power failures affected as many as 422,000 homes. Rain flooded crop fields, adding to damage from earlier storms. Saomai's developing rainbands had also caused damage in the Mariana Islands before its later passage toward East Asia.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Saomai (2000)

QUICK ANSWERS

Saomai in brief

What was Typhoon Saomai's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Sep 10, 2000, 12:00 PM UTC.

What category was Typhoon Saomai?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Sep 10, 2000, 12:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Saomai's lowest pressure?

925 mb, the minimum central pressure recorded during its tropical stage, on Sep 10, 2000, 12:00 PM UTC.

When did Typhoon Saomai occur?

The archived track runs from Aug 31, 2000, 06:00 PM UTC to Sep 19, 2000, 12:00 AM UTC, with the tropical stage from Aug 31, 2000, 06:00 PM UTC to Sep 16, 2000, 03:00 AM UTC.

Where did Typhoon Saomai form?

In the Western Pacific basin, in the 2000 season. Its first archived position is 13.5°N, 156.9°E on Aug 31, 2000, 06:00 PM UTC.

Did Typhoon Saomai make landfall?

The archive places its center over land at 1 recorded position; the strongest is 69 mph on Sep 15, 2000, 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