2012 Western Pacific typhoon season

Typhoon Bopha 2012

Bopha developed unusually close to the equator and struck Mindanao after reaching Category 5 strength. Known in the Philippines as Pablo, it caused widespread destruction across the island.

PEAK INTENSITYCategory 5
Satellite image of Bopha 2012
VIIRS Imagery from NOAA's Suomi-NPP Satellite, data superimposed with NASA's Blue Marble 2004. public domain Source
Bopha 2012: BOPHA infrared satellite image, 2012-12-04T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
BOPHA: complete recorded track, Nov 25, 2012–Dec 9, 2012Recorded track from Nov 25, 2012 to Dec 9, 2012. Colors show the recorded wind category. The highlighted position follows the replay controls.JAPANTAIWANVANUATUNov 26, 12:00 AM UTCNov 27, 12:00 AM UTCNov 28, 12:00 AM UTCNov 29, 12:00 AM UTCNov 30, 12:00 AM UTCDec 1, 12:00 AM UTCDec 2, 12:00 AM UTCDec 3, 12:00 AM UTCDec 4, 12:00 AM UTCDec 5, 12:00 AM UTCDec 6, 12:00 AM UTCDec 7, 12:00 AM UTCDec 8, 12:00 AM UTCDec 9, 12:00 AM UTCPeak: Category 5NOV 25DEC 9

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 173 mphPressure 911 mb
09001009602001020mphmbNov 25Nov 30Dec 4Dec 9
Forward speed 16 mphCumulative ACE 24.60 10⁴ kt²
0015203040mph10⁴ kt²Nov 25Nov 30Dec 4Dec 9
Maximum sustained wind173 mph

173 mph

Minimum recorded pressure911 hPa

Dec 3, 2012 during the tropical stage

Recorded track duration13.75 days

Full archive record, including non-tropical stages if present

Approximate track distance3,540 mi

Along the recorded center positions

STORM HISTORY

An unusually southerly typhoon

Bopha's archived track begins near 3 degrees north on November 25. The cyclone moved westward across the Caroline Islands and brought damage to Palau before approaching the Philippines. Its low-latitude route carried the powerful circulation toward Mindanao rather than the more frequently affected northern islands.

Sustained winds reached an archived peak of 150 knots on December 3. Bopha then struck eastern Mindanao late that day UTC, already December 4 locally. Davao Oriental and the area now called Davao de Oro were among the hardest-hit provinces.

Destruction across Mindanao

The typhoon crossed southern and central Mindanao, cutting power and triggering landslides. Thousands of residents lost their homes, and more than 170,000 people sought shelter in evacuation centers. The circulation continued toward Palawan and the South China Sea, where its later track ended on December 9.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Bopha

QUICK ANSWERS

Bopha in brief

What was Typhoon Bopha's highest wind speed?

173 mph, the highest one-minute sustained wind in its tropical stage, recorded on Dec 3, 2012, 06:00 PM UTC.

What category was Typhoon Bopha?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Dec 3, 2012, 12:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Bopha's lowest pressure?

911 mb, the minimum central pressure recorded during its tropical stage, on Dec 3, 2012, 06:00 PM UTC.

When did Typhoon Bopha occur?

The archived track runs from Nov 25, 2012, 12:00 PM UTC to Dec 9, 2012, 06:00 AM UTC, with the tropical stage from Nov 25, 2012, 12:00 PM UTC to Dec 9, 2012, 03:00 AM UTC.

Where did Typhoon Bopha form?

In the Western Pacific basin, in the 2012 season. Its first archived position is 3.4°N, 157.4°E on Nov 25, 2012, 12:00 PM UTC.

Did Typhoon Bopha make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 153 mph on Dec 3, 2012, 09:00 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