2009 Western Pacific typhoon season

Typhoon Choi-Wan 2009

Choi-Wan passed through the Northern Mariana Islands during rapid intensification. The small island of Alamagan suffered extensive destruction even though no casualties were reported.

PEAK INTENSITYCategory 5
Choi-Wan 2009: CHOI-WAN infrared satellite image, 2009-09-16T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
CHOI-WAN: complete recorded track, Sep 11, 2009–Sep 20, 2009Recorded track from Sep 11, 2009 to Sep 20, 2009. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANPHILIPPINESTAIWANSep 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 UTCSep 20, 12:00 AM UTCPeak: Category 5SEP 11SEP 20

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 918 mb
09001009602001020mphmbSep 11Sep 14Sep 17Sep 20
Forward speed 9 mphCumulative ACE 12.86 10⁴ kt²
002517.55035mph10⁴ kt²Sep 11Sep 14Sep 17Sep 20
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure918 hPa

Sep 15, 2009 during the tropical stage

Recorded track duration9.25 days

Full archive record, including non-tropical stages if present

Approximate track distance2,870 mi

Along the recorded center positions

STORM HISTORY

Strengthening through the Marianas

The cyclone developed east of Guam on September 11 and became Tropical Storm Choi-Wan the following day. It moved westward and intensified quickly, crossing the Northern Mariana Islands on September 15. The archive records its peak sustained winds of 140 knots later that day.

On Alamagan, the storm destroyed all but one structure and felled most trees. The United States Navy judged the island uninhabitable after the passage. Residents were evacuated to Saipan, despite the absence of reported storm deaths or injuries.

Loss of strength over open water

Choi-Wan remained powerful into September 17, when weakening outflow reduced support for its thunderstorms. An eyewall replacement cycle also altered the inner core. Stronger wind shear then accelerated weakening on September 19, and the storm became extratropical on September 20 over open water.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Choi-wan (2009)

QUICK ANSWERS

Choi-Wan in brief

What was Typhoon Choi-Wan's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Sep 15, 2009, 06:00 PM UTC.

What category was Typhoon Choi-Wan?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Sep 15, 2009, 03:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Choi-Wan's lowest pressure?

918 mb, the minimum central pressure recorded during its tropical stage, on Sep 15, 2009, 06:00 PM UTC.

When did Typhoon Choi-Wan occur?

The archived track runs from Sep 11, 2009, 12:00 PM UTC to Sep 20, 2009, 06:00 PM UTC, with the tropical stage from Sep 12, 2009, 12:00 AM UTC to Sep 20, 2009, 03:00 AM UTC.

Where did Typhoon Choi-Wan form?

In the Western Pacific basin, in the 2009 season. Its first archived position is 13.4°N, 155°E on Sep 11, 2009, 12:00 PM UTC.

Did Typhoon Choi-Wan make landfall?

No archived position places Typhoon Choi-Wan's center over land, but positions are six-hourly and a brief landfall can fall between them.

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