2012 Western Pacific typhoon season

Typhoon Sanba 2012

Sanba intensified rapidly east of the Philippines before moving north toward Japan and Korea. It weakened well before landfall, but heavy rain damaged roads and farmland across its later route.

PEAK INTENSITYCategory 5
Sanba 2012: SANBA infrared satellite image, 2012-09-14T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
SANBA: complete recorded track, Sep 10, 2012–Sep 18, 2012Recorded track from Sep 10, 2012 to Sep 18, 2012. Colors show the recorded wind category. The highlighted position follows the replay controls.AUSTRALIAASIAJAPANINDIAFIJITONGAVANUATUNEW CALEDONIAMAURITIUSPacific OceanIndian OceanSep 10, 12:00 AM UTCSep 11, 12:00 AM UTCSep 12, 12:00 AM UTCSep 13, 12:00 AM UTCSep 14, 12:00 AM UTCSep 15, 12:00 AM UTCSep 16, 12:00 AM UTCSep 17, 12:00 AM UTCSep 18, 12:00 AM UTCPeak: Category 5SEP 10SEP 18

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 178 mphPressure 907 mb
09001009602001020mphmbSep 10Sep 12Sep 15Sep 18
Forward speed 10 mphCumulative ACE 8.91 10⁴ kt²
0020154030mph10⁴ kt²Sep 10Sep 12Sep 15Sep 18
Maximum sustained wind178 mph

178 mph

Minimum recorded pressure907 hPa

Sep 13, 2012 during the tropical stage

Recorded track duration8.75 days

Full archive record, including non-tropical stages if present

Approximate track distance2,990 mi

Along the recorded center positions

STORM HISTORY

Rapid intensification on a northward track

Sanba developed on September 10 and became a typhoon two days later. Favorable conditions then supported rapid strengthening. The archive records peak sustained winds of 155 knots on September 13, equivalent to Category 5 strength on the one-minute wind scale.

The eye expanded as Sanba moved toward higher latitudes and gradually weakened. It passed west of Japan and reached South Korea on September 17. The circulation then lost its tropical structure, with remnants continuing toward Russia's Primorsky Krai region.

Rainfall damage in Japan and Korea

Sanba damaged agriculture, forestry and fishing in Okinawa Prefecture. Farther north in Japan, heavy rain washed out roads and flooded agricultural areas. South Korea also suffered flooded cropland and damaged infrastructure, with losses estimated at 365.7 billion won. In North Korea, the rainfall worsened flooding that had begun earlier in the season.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Typhoon Sanba

QUICK ANSWERS

Sanba in brief

What was Typhoon Sanba's highest wind speed?

178 mph, the highest one-minute sustained wind in its tropical stage, recorded on Sep 13, 2012, 06:00 PM UTC.

What category was Typhoon Sanba?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Sep 13, 2012, 12:00 PM UTC. Other agencies classify storms differently.

What was Typhoon Sanba's lowest pressure?

907 mb, the minimum central pressure recorded during its tropical stage, on Sep 13, 2012, 06:00 PM UTC.

When did Typhoon Sanba occur?

The archived track runs from Sep 10, 2012, 12:00 AM UTC to Sep 18, 2012, 06:00 PM UTC, with the tropical stage from Sep 10, 2012, 12:00 AM UTC to Sep 17, 2012, 09:00 AM UTC.

Where did Typhoon Sanba form?

In the Western Pacific basin, in the 2012 season. Its first archived position is 8.6°N, 134.8°E on Sep 10, 2012, 12:00 AM UTC.

Did Typhoon Sanba make landfall?

The archive places its center over land at 1 recorded position; the strongest is 75 mph on Sep 17, 2012, 03:00 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