2009 Western Pacific typhoon season

Typhoon Melor 2009

Melor reached Category 5 strength in the western Pacific before turning toward Japan. Along the way, its interaction with Typhoon Parma helped keep that storm near northern Luzon.

PEAK INTENSITYCategory 5
Satellite image of Melor 2009
NASA. public domain Source
Melor 2009: MELOR infrared satellite image, 2009-10-04T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
MELOR: complete recorded track, Sep 28, 2009–Oct 11, 2009Recorded track from Sep 28, 2009 to Oct 11, 2009. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAASIAPHILIPPINESINDIATAIWANFIJITONGAVANUATUNEW CALEDONIAPacific OceanIndian OceanSep 29, 12:00 AM UTCSep 30, 12:00 AM UTCOct 1, 12:00 AM UTCOct 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 UTCOct 11, 12:00 AM UTCPeak: Category 5SEP 28OCT 11

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 173 mphPressure 911 mb
09001009602001020mphmbSep 28Oct 2Oct 6Oct 11
Forward speed 17 mphCumulative ACE 20.80 10⁴ kt²
002522.55045mph10⁴ kt²Sep 28Oct 2Oct 6Oct 11
Maximum sustained wind173 mph

173 mph

Minimum recorded pressure911 hPa

Oct 4, 2009 during the tropical stage

Recorded track duration12.5 days

Full archive record, including non-tropical stages if present

Approximate track distance5,710 mi

Along the recorded center positions

STORM HISTORY

Rapid intensification and a nearby typhoon

Melor developed into a tropical depression on September 29 and strengthened rapidly during the first days of October. Favorable outflow allowed the storm's thunderstorms to organize around its center. Sustained winds reached an archived maximum of 150 knots on October 4.

As Melor moved northwestward, it interacted with Parma near the Philippines. The circulation around the two storms helped hold Parma near northern Luzon, prolonging heavy rainfall there. Melor itself continued toward Japan while gradually losing strength.

Japan and the North Pacific

Melor reached Japan on October 7 UTC and became extratropical as it crossed the country. The saved account reports three deaths and approximately US$1.5 billion in damage in Japan, measured in 2009 dollars.

Its remnants continued across the North Pacific and were absorbed into another low near Alaska. That developing system later strengthened and affected the western United States, extending the meteorological history of Melor's remnants beyond its tropical lifetime.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Melor (2009)

QUICK ANSWERS

Melor in brief

What was Typhoon Melor's highest wind speed?

173 mph, the highest one-minute sustained wind in its tropical stage, recorded on Oct 4, 2009, 06:00 AM UTC.

What category was Typhoon Melor?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Oct 3, 2009, 09:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Melor's lowest pressure?

911 mb, the minimum central pressure recorded during its tropical stage, on Oct 4, 2009, 06:00 AM UTC.

When did Typhoon Melor occur?

The archived track runs from Sep 28, 2009, 12:00 PM UTC to Oct 11, 2009, 12:00 AM UTC, with the tropical stage from Sep 29, 2009, 06:00 AM UTC to Oct 8, 2009, 03:00 AM UTC.

Where did Typhoon Melor form?

In the Western Pacific basin, in the 2009 season. Its first archived position is 7.3°N, 163.8°E on Sep 28, 2009, 12:00 PM UTC.

Did Typhoon Melor make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 72 mph on Oct 7, 2009, 07:00 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