Late on October 10, a tropical disturbance formed east-southeast of
Guam. There were favorable environmental conditions, such as low vertical
wind shear, good upper-level
divergence and poleward
outflow. The system began to significantly develop on October 12, prompting the
Joint Typhoon Warning Center (JTWC) issuing a
Tropical Cyclone Formation Alert at 09:00
UTC. Several hours later, the
Japan Meteorological Agency (JMA) began monitoring the system as a tropical depression. Early on October 13, JTWC also classified the system as a tropical depression and designated it
15W. Hours later, well-defined
convective banding features developed around the system and thunderstorm activity over the center of circulation increased.
Sea surface temperatures above and high
oceanic heat content allowed for further strengthening. Situated to the southwest of a
subtropical ridge, the system slowly tracked west-northwest towards the
Philippines. Around 12:00
UTC, the system further intensified into a tropical storm, earning the name
Megi from JMA. Late on October 13, Tropical Storm Megi became quasi-stationary, but a mid-latitude
trough moving from the west caused the storm to resume a northwestward track around the periphery of the subtropical ridge. Throughout the morning of October 14, a
central dense overcast developed over the center of Megi, allowing for intensification. Later that day, microwave imagery showed a developing mid-level
eye feature, resulting in JMA upgrading the system to a severe tropical storm and JTWC upgrading it to a typhoon. Around this time, Megi began to be observed by
Hurricane Hunters from the
United States Air Force's (USAF)
53rd Weather Reconnaissance Squadron, as part of a field campaign researching typhoon impacts on the ocean. On their first flight, they verified the microwave data of a developing eye within the cyclone. On October 15, JMA upgraded Megi to a typhoon, and the
Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) began to mention the typhoon and named it
Juan as it entered the
Philippine Area of Responsibility, with improved outflow over the western semi-circle and a well-defined low-level circulation center with tightly curved banding; steady intensification continued thereafter. By the afternoon of October 16, Megi began to undergo
rapid intensification with a well-defined eye developing, and enhanced poleward outflow developing due to a transitory mid-latitude
trough. Early on October 17, Megi started to moved westward and then west-southwestward because of the
subtropical ridge. Based on aircraft data, increased satellite estimates and a circular diameter eye, JTWC upgraded Megi to a category 5-equivalent
super typhoon on the
Saffir–Simpson hurricane wind scale, becoming the only super typhoon in 2010. Hurricane Hunters later that morning found Megi to have become extremely intense, measuring near-record-high
flight-level winds of , while the
Stepped-Frequency Microwave Radiometer (SFMR) found surface winds near , in addition to the pressure dropping to . They also noted that there was frequent
lightning within Megi's
eyewall. Additionally, a
dropsonde recorded a maximum
wind gust aloft of ; this stood as a world record until surpassed by the
North Atlantic's
Hurricane Melissa in
2025 fifteen years later. Based on the measurements, the JTWC set Megi's maximum intensity at 295 km/h (185 mph), although the pressure was listed in post-analysis as nearly higher than what the Hurricane Hunters actually observed. though Megi remained steady in intensity until it made landfall over
Isabela, Philippines at 03:25
UTC (11:25
PST) on October 18. When passing the
Sierra Madre, the eye filled due to land interaction, but tightly curved banding and excellent radial outflow remained. The weakened typhoon emerged into the
South China Sea late on October 18, and it began to reorganize. On October 19, Megi formed an enlarged but ragged eye. Late on the same day, Megi turned northwestward and moved slowly due to the significantly weakening western
subtropical ridge in response to a deepening mid-latitude shortwave
trough moving into Southeast
China. Megi turned northward then north-northeastward towards a break in the
subtropical ridge caused by an approaching mid-latitude
trough on October 20. By low vertical
wind shear and good radial outflow especially on the poleward channel, the typhoon started to gradually intensify. On October 21, JMA reported that Megi attained its secondary peak intensity by the 10-minute maximum sustained winds reaching and the atmospheric pressure decreasing to . On October 22, the eye of Typhoon Megi became cloud-filled and convection begun eroding due to increasing vertical
wind shear. Late on the same day, JMA downgraded Megi to a severe tropical storm in the
Taiwan Strait because of
subsidence induced by a developing upper-level
trough west of the storm. On October 23, Megi made landfall over
Zhangpu in
Fujian,
China at 04:55 UTC. Soon, Megi weakened to a tropical storm in
mainland China, as the majority of convection associated with the system has dissipated, prompting JTWC issuing a final warning. Megi further weakened to a tropical depression late on October 23. On October 24, the tropical depression dissipated completely around 12:00 UTC, though according to the JTWC Best Track Data analysis, Megi became extratropical at 00:00 UTC on the next day.
Records The
Japan Meteorological Agency (JMA) analysed that the 10-minute maximum sustained winds of Typhoon Megi in 2010 was , making it the second strongest tropical cyclone in the Northwest Pacific Ocean on record along with
Bess in 1982 and
Haiyan in 2013, only after
Tip in 1979. The
Hong Kong Observatory analysed that Megi was the strongest tropical cyclone in the Northwest Pacific Ocean since Tip in 1979 by attaining the 10-minute maximum sustained winds at 270 km/h (145 knots, 165 mph). A
hurricane hunter aircraft indicated 1-minute maximum sustained surface winds of and minimum pressure was at peak intensity, which was equivalent to Tip in 1979. According to JMA's advisory, Megi still maintained its peak strength at 03:00 UTC on October 18, making it one of the strongest tropical cyclones to make landfall on record at 03:25 UTC. Moreover, Megi was the latest-forming storm to make landfall over
Fujian, China since 1949. In addition, a dropsonde positioned in the eyewall recorded a wind gust of , which was the highest wind speed ever measured by dropsonde until the North Atlantic's
Hurricane Melissa surpassed it in 2025. ==Preparations==