2004 Western Pacific typhoon season

Typhoon Ma-On 2004

Typhoon Ma-On struck the Izu Peninsula in October 2004 and produced record winds around parts of the Tokyo region. Local terrain intensified winds behind the center as the storm crossed eastern Japan.

PEAK INTENSITYCategory 5
Satellite image of Ma-On 2004
Moderate Resolution Imaging Spectroradiometer (MODIS) image from NASA's Terra satellite. public domain Source
Ma-On 2004: MA-ON infrared satellite image, 2004-10-08T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
MA-ON: complete recorded track, Oct 1, 2004–Oct 10, 2004Recorded track from Oct 1, 2004 to Oct 10, 2004. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAPHILIPPINESTAIWANOct 2, 12:00 AM UTCOct 3, 12:00 AM UTCOct 4, 12:00 AM UTCOct 5, 12:00 AM UTCOct 6, 12:00 AM UTCOct 7, 12:00 AM UTCOct 8, 12:00 AM UTCOct 9, 12:00 AM UTCOct 10, 12:00 AM UTCPeak: Category 5OCT 1OCT 10

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 898 mb
08801009502001020mphmbOct 1Oct 4Oct 7Oct 10
Forward speed 13 mphCumulative ACE 9.42 10⁴ kt²
0030106020mph10⁴ kt²Oct 1Oct 4Oct 7Oct 10
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure898 hPa

Oct 8, 2004 during the tropical stage

Recorded track duration8.75 days

Full archive record, including non-tropical stages if present

Approximate track distance2,650 mi

Along the recorded center positions

STORM HISTORY

Strengthening during a turn toward Japan

Ma-On developed from a weak low northwest of Guam and spent several days organizing. It became a tropical storm on October 4, then a typhoon as it moved north and northwest. An approaching trough turned it northeast and improved its upper-level outflow, supporting rapid strengthening.

Maximum one-minute winds reached 140 kt on October 8. Ma-On weakened as it accelerated toward Japan, making landfall on the Izu Peninsula on October 9. It crossed the country and returned to the Pacific within about six hours, then completed its extratropical transition.

Terrain-enhanced winds and transport disruption

Observers at Irozaki measured a gust of 243 km/h. Around Sagami Bay, some of the strongest winds occurred behind the storm as cool air flowed south along the Kanto Mountains. This terrain-related wind pattern caused damage beyond what the broad storm circulation alone would suggest.

Officials ordered thousands of families to evacuate. Airlines canceled hundreds of flights, and railway operators suspended the Tokaido Shinkansen. The storm also delayed Japanese Grand Prix qualifying at Suzuka. The saved account records seven deaths and two missing people.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Ma-on (2004)

QUICK ANSWERS

Ma-On in brief

What was Typhoon Ma-On's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Oct 8, 2004, 12:00 AM UTC.

What category was Typhoon Ma-On?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Oct 8, 2004, 12:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Ma-On's lowest pressure?

898 mb, the minimum central pressure recorded during its tropical stage, on Oct 8, 2004, 12:00 AM UTC.

When did Typhoon Ma-On occur?

The archived track runs from Oct 1, 2004, 06:00 AM UTC to Oct 10, 2004, 12:00 AM UTC, with the tropical stage from Oct 4, 2004, 12:00 AM UTC to Oct 9, 2004, 09:00 PM UTC.

Where did Typhoon Ma-On form?

In the Western Pacific basin, in the 2004 season. Its first archived position is 14.3°N, 138.6°E on Oct 1, 2004, 06:00 AM UTC.

Did Typhoon Ma-On make landfall?

The archive places its center over land at 1 recorded position; the strongest is 109 mph on Oct 9, 2004, 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