Typhoon Nari (2013)

[citation needed] On October 8, 2013 the Japan Meteorological Agency (JMA) started to monitor a tropical depression, that developed within an area of low to moderate vertical windshear, about 1,150 km (715 mi) to the east of Manila on the Philippine island of Luzon.

[1][2] The system was subsequently named Santi by the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) as it moved along the southern edge of a subtropical ridge of high pressure.

[3] During the next day after central convection over the systems low level circulation centre had increased both the JMA and the JTWC reported that the depression had developed into a tropical storm, with the latter naming it as Nari.

[1][5] Nari ensued a period of rapid intensification in the Philippine Sea, with the Japan Meteorological Agency and PAGASA upgrading the system into a typhoon.

[12] During October 11, the areas under signal 3 were expanded to include Benguet, Ifugao, Ilocos Sur, Isabela, La Union, Pangasinan, Polillo Island, Quirino, Nueva Ecija and Tarlac.

[18] On October 16, poor weather from the remnants of Typhoon Nari has been cited as a probable cause for the crash of Lao Airlines Flight 301, on approach to Pakse International Airport with the loss of all 49 passengers and crew.

Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
Map key
Tropical depression (≤38 mph, ≤62 km/h)
Tropical storm (39–73 mph, 63–118 km/h)
Category 1 (74–95 mph, 119–153 km/h)
Category 2 (96–110 mph, 154–177 km/h)
Category 3 (111–129 mph, 178–208 km/h)
Category 4 (130–156 mph, 209–251 km/h)
Category 5 (≥157 mph, ≥252 km/h)
Unknown
Storm type
triangle Extratropical cyclone , remnant low, tropical disturbance, or monsoon depression
Damages in Vietnam