Typhoon Sepat (2007)

Map plotting the track and the intensity of the storm, according to the Saffir–Simpson scale

On August 11, a low-level circulation center formed in conjunction with a persistent area of convection about 1,280 km (800 mi) southeast of Naha, Okinawa. Northerly upper-level winds initially provided beneficial divergence, though also resulted in detrimental wind shear and lack of inflow.[1] Upper-level conditions gradually became more favorable for development as the disturbance tracked along the eastern periphery of an upper-level anticyclone. With convective rain bands wrapping into the circulation, the Joint Typhoon Warning Center (JTWC) issued a tropical cyclone formation alert on the system late on August 11.[2] Remaining nearly stationary between ridges to its northeast and southwest, the system developed further, and early on August 12 the JTWC classified it as Tropical Depression 09W.[3] Shortly thereafter, the Japan Meteorological Agency (JMA) classified it as a tropical depression while located about 1,245 km (774 mi) southeast of Okinawa.[4]

Twelve hours later, the JTWC upgraded the tropical depression to a tropical storm[5] based on Dvorak technique satellite intensity estimates and[6] the storm exhibiting tightly-curved convective bands. An upper-level low helped to reduce wind shear that had been affecting the storm.[6] The JTWC also warned of the possibility of rapid intensification.[6] The JMA upgraded the depression to a tropical storm later that day[7] and named it Sepat, a name contributed by Malaysia referring to a freshwater fish species.[8]

By early the next morning, August 13, Sepat had a banding eye visible on microwave satellite imagery[9] and had remained in an environment conducive for strengthening, including weakening wind shear. An upper-level anticyclone also moved over the storm.[9] By now, Sepat had moved into PAGASA's area of responsibility and attained the local name "Egay". The JMA upgraded Sepat to a severe tropical storm shortly after.[10] Sepat continued to slowly gain more organisation and intensify further,[11] and started to move faster under the influence of a subtropical steering ridge.[11] Sepat strengthened into a typhoon on the morning of August 14[12][13] under still-decreasing wind shear and favourable diffluence.[14]

Sepat developed a cloud-filled eye measuring 12 nautical miles (22 km; 14 mi) across by later that night, part of a larger central dense overcast nearly 130 nmi (240 km), 150 mi) wide.[15] Favourable sea surface temperatures of 29–30 °C (84–86 °F) allowed Sepat to continue intensifying despite decrease of poleward outflow.[15] By this time, Sepat had deepened to 955 hPa.[16] The JTWC also noted possible imminent rapid intensification of the storm.[15]

Late that night, Sepat underwent rapid intensification as expected, and was upgraded by the JTWC to a super typhoon the next morning.[17] The JMA analysed Sepat at 940 hPa at the same time.[18] The deep convection warmed slightly and underwent slight fluctuations during the afternoon.[19] During this period, Sepat slowed in forward speed and took a turn from a west-southwest motion to a more poleward one.[20] Its eye also cleared out, became slightly larger, and warmed.[20] By late that night, Sepat had become the strongest storm of the season to date, with the JMA analysing its pressure at 925 hPa,[21] lower than Typhoon Man-yi's minimum of 935 hPa.

Typhoon Sepat during an eyewall replacement cycle on August 17

Continuing to intensify,[22] Sepat reached a peak minimum central pressure of 910 hPa on the morning of August 16.[23] It also managed to maintain its cloud-free eye.[22] High ocean heat content and good equatorward outflow allowed Sepat to maintain its intensity, but an eyewall replacement cycle began later that night.[24] The eyewall replacement cycle continued throughout the night, and by the next morning Sepat displayed concentric eyewalls, with the inner eyewall being weaker.[25] The JTWC downgraded it to a typhoon later that evening.[26]

It made landfall in eastern Taiwan between Taitung and Hualien on the morning of August 18 local time at around 5 a.m. (2100 UTC August 17)[27] and weakened to a minimal typhoon.[28] After crossing the island, Sepat held on to minimal typhoon intensity before weakening to a severe tropical storm that night.[29] It made a second landfall, in China, about 24 hours after landfall on Taiwan and was downgraded to a tropical storm the next morning. It further weakened inland and the JMA issued its final advisory on the morning of August 20.

The Government of the Republic of China issued sea typhoon warnings on the morning of August 16 and land warnings later that evening.[30] At all county and city levels, a typhoon holiday was declared for August 18 in preparation for the storm. In the Philippines, PAGASA issued Public Storm Warning Signals 1 to 3 (4 is the highest signal) for most provinces of Luzon.[31]

Over 900,000 people were evacuated in eastern China, and over 100 flights had to be cancelled.[32] In Taiwan, nearly 2,000 people had to be evacuated.[33]

After Sepat made landfall in China, the regional meteorological office in Hunan Province sent over 2.25 million text messages to residents to warn them about the storm's remnants.[34]

• Typhoon Kalmaegi (2008)
• Typhoon Matmo (2014)
• Typhoon Chan-hom (2015)
• Typhoon Nepartak (2016)

Wikimedia Commons has media related to Typhoon Sepat (2007).

• JMA General Information of Typhoon Sepat (0708) from Digital Typhoon
• JMA Best Track Data of Typhoon Sepat (0808) (in Japanese)
• JMA Best Track Data (Graphics) of Typhoon Sepat (0708)
• JMA Best Track Data (Text)
• JTWC Best Track Data of Super Typhoon 09W (Sepat)
• 09W.SEPAT from the U.S. Naval Research Laboratory