2010 South Pacific cyclone season

Cyclone Ului 2010

Ului intensified from a tropical storm to Category 5 strength within about 30 hours. It later crossed the Coral Sea and struck Queensland at a much lower intensity.

PEAK INTENSITYCategory 5
Satellite image of Ului 2010
NASA/ MODIS Rapid Response System. public domain Source
Ului 2010: ULUI infrared satellite image, 2010-03-14T18:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
ULUI: complete recorded track, Mar 10, 2010–Mar 22, 2010Recorded track from Mar 10, 2010 to Mar 22, 2010. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIANEW CALEDONIAMar 11, 12:00 AM UTCMar 12, 12:00 AM UTCMar 13, 12:00 AM UTCMar 14, 12:00 AM UTCMar 15, 12:00 AM UTCMar 16, 12:00 AM UTCMar 17, 12:00 AM UTCMar 18, 12:00 AM UTCMar 19, 12:00 AM UTCMar 20, 12:00 AM UTCMar 21, 12:00 AM UTCMar 22, 12:00 AM UTCPeak: Category 5MAR 10MAR 22

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 918 mb
09001009602001020mphmbMar 10Mar 14Mar 18Mar 22
Forward speed 7 mphCumulative ACE 6.98 10⁴ kt²
001017.52035mph10⁴ kt²Mar 10Mar 14Mar 18Mar 22
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure918 hPa

Mar 14, 2010 during the tropical stage

Recorded track duration11.5 days

Full archive record, including non-tropical stages if present

Approximate track distance2,100 mi

Along the recorded center positions

STORM HISTORY

Rapid intensification near Vanuatu

Ului's precursor was identified north of Hiw Island, Vanuatu, in early March. The developing circulation moved slowly westward, with thunderstorms and curved rainbands becoming better organized. It received its name on March 12 and strengthened rapidly over the next two days.

The archive records peak sustained winds of 140 knots on March 14. Ului then weakened while continuing into the Coral Sea. Its intensity declined for several days before a final increase as the cyclone approached Australia.

Through the Whitsundays to Queensland

Ului crossed the outer Whitsunday Islands and made landfall near Airlie Beach early on March 21 local time. It was classified as Category 3 on the Australian cyclone scale at the coast, a different scale from the one-minute wind categories used in the track display.

Queensland's agricultural losses were estimated at A$60 million, with a further A$20 million in infrastructure damage. The substantial farm losses made agriculture the largest part of the reported damage bill.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Cyclone Ului

QUICK ANSWERS

Ului in brief

What was Cyclone Ului's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Mar 14, 2010, 12:00 AM UTC.

What category was Cyclone Ului?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Mar 14, 2010, 12:00 AM UTC. Other agencies classify storms differently.

What was Cyclone Ului's lowest pressure?

918 mb, the minimum central pressure recorded during its tropical stage, on Mar 14, 2010, 12:00 AM UTC.

When did Cyclone Ului occur?

The archived track runs from Mar 10, 2010, 12:00 PM UTC to Mar 22, 2010, 12:00 AM UTC, with the tropical stage from Mar 10, 2010, 06:00 PM UTC to Mar 21, 2010, 09:00 PM UTC.

Where did Cyclone Ului form?

In the South Pacific basin, in the 2010 season. Its first archived position is 14.6°S, 168°E on Mar 10, 2010, 12:00 PM UTC.

Did Cyclone Ului make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 78 mph on Mar 20, 2010, 04:00 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