2015 Western Pacific typhoon season

Typhoon Atsani 2015

Atsani developed near the Marshall Islands and strengthened into a powerful offshore typhoon. Its track curved northeastward as dry air and increasing wind shear weakened the core.

PEAK INTENSITYCategory 5
Satellite image of Atsani 2015
NASA, LANCE / MODIS on Aqua. public domain Source
Atsani 2015: ATSANI infrared satellite image, 2015-08-19T03:00:00Z
Digital Typhoon, National Institute of Informatics (doi:10.20783/DIAS.664). CC BY 4.0 Source
ATSANI: complete recorded track, Aug 14, 2015–Aug 29, 2015Recorded track from Aug 14, 2015 to Aug 29, 2015. Colors show the recorded wind category. The highlighted position follows the replay controls.ASIAJAPANPHILIPPINESTAIWANFIJIVANUATUPacific OceanAug 14, 12:00 AM UTCAug 15, 12:00 AM UTCAug 16, 12:00 AM UTCAug 17, 12:00 AM UTCAug 18, 12:00 AM UTCAug 19, 12:00 AM UTCAug 20, 12:00 AM UTCAug 21, 12:00 AM UTCAug 22, 12:00 AM UTCAug 23, 12:00 AM UTCAug 24, 12:00 AM UTCAug 25, 12:00 AM UTCAug 26, 12:00 AM UTCAug 27, 12:00 AM UTCAug 28, 12:00 AM UTCAug 29, 12:00 AM UTCPeak: Category 5AUG 14AUG 29

Drag to pan. Pinch or Ctrl/⌘ + scroll to zoom. Keyboard: plus or minus to zoom, arrow keys to pan, and 0 to show the full track.

DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 918 mb
09001009602001020mphmbAug 14Aug 19Aug 24Aug 29
Forward speed 12 mphCumulative ACE 17.40 10⁴ kt²
0020204040mph10⁴ kt²Aug 14Aug 19Aug 24Aug 29
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure918 hPa

Aug 19, 2015 during the tropical stage

Recorded track duration15.25 days

Full archive record, including non-tropical stages if present

Approximate track distance3,780 mi

Along the recorded center positions

STORM HISTORY

A well-organized offshore peak

Atsani's precursor was monitored north-northwest of Wotje Atoll before becoming a depression and named storm on August 14. A developing eye marked its transition to a typhoon on August 16. Over the following days, the rainbands tightened and the central thunderstorms deepened.

Very low wind shear and strong outflow supported further intensification. Archived sustained winds reached 140 knots on August 19, when Atsani had a broad, sharply defined eye. The cyclone then weakened while continuing northwestward.

Dry air and a northeastward turn

An eyewall replacement cycle changed the core as dry air entered the circulation and wind shear increased. Atsani turned northeastward, falling below typhoon strength on August 24. It became extratropical northeast of Japan on August 25. No archived position places the center over land, and the later track continues into August 29.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, 2015 Pacific typhoon season, Atsani section

QUICK ANSWERS

Atsani in brief

What was Typhoon Atsani's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Aug 19, 2015, 12:00 PM UTC.

What category was Typhoon Atsani?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Aug 19, 2015, 09:00 AM UTC. Other agencies classify storms differently.

What was Typhoon Atsani's lowest pressure?

918 mb, the minimum central pressure recorded during its tropical stage, on Aug 19, 2015, 12:00 PM UTC.

When did Typhoon Atsani occur?

The archived track runs from Aug 14, 2015, 12:00 AM UTC to Aug 29, 2015, 06:00 AM UTC, with the tropical stage from Aug 14, 2015, 12:00 AM UTC to Aug 24, 2015, 09:00 PM UTC.

Where did Typhoon Atsani form?

In the Western Pacific basin, in the 2015 season. Its first archived position is 14.8°N, 163.5°E on Aug 14, 2015, 12:00 AM UTC.

Did Typhoon Atsani make landfall?

No archived position places Typhoon Atsani'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