Typhoon Wipha (2013)
Typhoon Wipha at peak intensity on October 13  | |
| Meteorological history | |
|---|---|
| Formed | October 9, 2013 | 
| Post-tropical | October 16, 2013 | 
| Dissipated | October 22, 2013 | 
| Very strong typhoon | |
| 10-minute sustained (JMA) | |
| Highest winds | 165 km/h (105 mph) | 
| Lowest pressure | 930 hPa (mbar); 27.46 inHg | 
| Category 4-equivalent typhoon | |
| 1-minute sustained (SSHWS/JTWC) | |
| Highest winds | 220 km/h (140 mph) | 
| Lowest pressure | 933 hPa (mbar); 27.55 inHg | 
| Overall effects | |
| Fatalities | 41 total | 
| Damage | $404.8 million (2013 USD) | 
| Areas affected | Northern Mariana Islands, Guam, Japan, Russian Far East, Alaska | 
| IBTrACS | |
Part of the 2013 Pacific typhoon season  | |
Typhoon Wipha, known in the Philippines as Typhoon Tino, was a large typhoon that caused extensive damage in Japan in mid-October 2013. The system originated from a tropical depression well to the east of Guam on October 8. Tracking generally westward, development of the depression was initially slow; however, on October 11, favorable atmospheric conditions allowed for rapid intensification. The depression strengthened to a tropical storm that day, receiving the name Wipha at the time, and reached typhoon status on October 12. Now moving northwestward, Wipha grew into a very large system and ultimately attained its peak intensity on October 14 with winds of 165 km/h (105 mph) and an atmospheric pressure of 930 mbar (hPa; 27.46 inHg). Accelerating and turning more northerly, the typhoon weakened as conditions became less conducive for tropical cyclones. Wipha dramatically accelerated northeastward on October 15 as it interacted with a stalled out front over Japan. Simultaneously, the storm began transitioning into an extratropical cyclone, a process which it completed early on October 16.