2011 Western Pacific typhoon season

Typhoon Songda 2011

Songda remained offshore while bringing damaging rain to the Philippines and strong winds to Okinawa. The typhoon reached Category 5 strength before weakening on its way toward Japan.

PEAK INTENSITYCategory 5
Songda 2011: SONGDA infrared satellite image, 2011-05-26T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
SONGDA: complete recorded track, May 19, 2011–Jun 2, 2011Recorded track from May 19, 2011 to Jun 2, 2011. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAFIJITONGAVANUATUNEW CALEDONIAPacific OceanMay 20, 12:00 AM UTCMay 21, 12:00 AM UTCMay 22, 12:00 AM UTCMay 23, 12:00 AM UTCMay 24, 12:00 AM UTCMay 25, 12:00 AM UTCMay 26, 12:00 AM UTCMay 27, 12:00 AM UTCMay 28, 12:00 AM UTCMay 29, 12:00 AM UTCMay 30, 12:00 AM UTCMay 31, 12:00 AM UTCJun 1, 12:00 AM UTCJun 2, 12:00 AM UTCPeak: Category 5MAY 19JUN 2

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 918 mb
09001009602001020mphmbMay 19May 24May 28Jun 2
Forward speed 12 mphCumulative ACE 13.02 10⁴ kt²
0025155030mph10⁴ kt²May 19May 24May 28Jun 2
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure918 hPa

May 26, 2011 during the tropical stage

Recorded track duration13.25 days

Full archive record, including non-tropical stages if present

Approximate track distance5,300 mi

Along the recorded center positions

STORM HISTORY

From Yap to a powerful typhoon

Songda organized southeast of Yap in May. Observations from the island led forecasters to revise an early estimate of its strength downward, but the system became an established tropical storm on May 21. It moved northwestward and was named Chedeng within the Philippine monitoring area.

The cyclone reached typhoon strength on May 24 and then intensified rapidly. Its archived sustained winds peaked at 140 knots on May 26. The center stayed offshore as the storm continued northward, eventually losing its tropical structure south of Shikoku on May 29.

Flooding and damaging winds offshore

Outer rainbands caused flash floods and landslides in the Philippines, where four deaths were attributed to Songda. Farther north, Okinawa experienced intense gusts and heavy rain, with losses estimated at 23.2 billion yen. Rain spread from Kyushu toward eastern Honshu as the system became extratropical, producing further flooding.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 2011 Pacific typhoon season, Songda section

QUICK ANSWERS

Songda in brief

What was Typhoon Songda's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on May 26, 2011, 06:00 AM UTC.

What category was Typhoon Songda?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on May 26, 2011, 06:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Songda's lowest pressure?

918 mb, the minimum central pressure recorded during its tropical stage, on May 26, 2011, 06:00 AM UTC.

When did Typhoon Songda occur?

The archived track runs from May 19, 2011, 06:00 PM UTC to Jun 2, 2011, 12:00 AM UTC, with the tropical stage from May 19, 2011, 06:00 PM UTC to May 29, 2011, 03:00 AM UTC.

Where did Typhoon Songda form?

In the Western Pacific basin, in the 2011 season. Its first archived position is 8.3°N, 141.6°E on May 19, 2011, 06:00 PM UTC.

Did Typhoon Songda make landfall?

No archived position places Typhoon Songda'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