Typhoon Krathon

Krathon, which refers to the santol fruit, was the first storm to make landfall on Taiwan's densely populated western plains since Typhoon Thelma in 1977.

Additionally, it was the wettest tropical cyclone in Basco, Batanes, bringing more than two months' worth of rainfall for September and surpassing the previous record set by Typhoon Ruth in 1991.

Early on October 1, the JMA reported that the storm had reached its peak intensity, with ten-minute sustained winds of 195 km/h (120 mph) and a central pressure of 920 hPa (27.17 inHg).

Once the eyewall replacement cycle was complete, Krathon began warming cloud tops and displayed a weakened cloud-filled eye feature that caused upwelling and a decrease in ocean heat content.

Ahead of the storm, a Tropical Cyclone Wind Signal was issued for various areas in the Philippines, with a red alert for Calayan and Santa Ana in Cagayan.

The origins of Typhoon Krathon can be traced back to September 26, when the Japan Meteorological Agency (JMA) reported a tropical depression 250 km (155 mi) south-southwest of Kadena Air Base, Japan,[1] characterised by a partially exposed low-level circulation centre with persistent deep convection in the southern semicircle and formative banding to the north.

[2][3] The United States Joint Typhoon Warning Center (JTWC) issued a tropical cyclone formation alert on September 27, noting that convective banding was wrapping into the centre and that the environmental analysis indicated a favourable environment for development due to low vertical wind shear, good equatorward outflow aloft, and warm sea surface temperatures of 29–30 °C (84–86 °F).

[7] Satellite imagery indicated that the storm was steadily consolidating, with spiral bands of deep convection extending across three quadrants of the system and encircling the low-level circulation centre.

[11]At around 18:00 UTC, the JMA upgraded the system to a severe tropical storm, utilizing the Dvorak technique to assess its intensity based on satellite imagery.

[13] Early the next day, both the JMA and the JTWC upgraded it to a minimal typhoon after it had opened a broad, raggedly-defined eye,[14][15] which had since become cloud-filled, and the system was moving north-northwestward between two mid-level subtropical high.

[16] On September 30, the eye of the typhoon, measuring 23 miles (37 km) in diameter, was visible on infrared satellite imagery,[17] surrounded by warm temperatures of 54–57 °F (12–14 °C),[18] as the storm gradually moved west-northwestward and passed near Sabtang, Batanes.

[21] Early on October 1, the JMA upgraded Krathon to a violent typhoon, estimating its peak intensity with a minimum central pressure of 920 hPa (27.17 inHg) and 10-minute maximum sustained winds of 195 km/h (120 mph).

[22] As it moved into the northern area of the South China Sea,[23] the cloud top temperatures of Krathon sharply decreased over the past six hours amid warm conditions.

[27] The following day, satellite imagery revealed that the system remained symmetrical; however, warming cloud tops became exposed due to increasing vertical wind shear.

[33] The JTWC discontinued warnings on the system as it moved inland, where the rugged southeastern mountain ranges of Taiwan eroded much of the deep convection associated with the circulation center as it weakened to a tropical depression.

[36] The JMA continued to monitor the system as it emerged into the South China Sea,[37] where it remained nearly stationary between two mid-level subtropical high before dissipating on the same day.

The Central Emergency Operation Center advised against traveling to coastal and mountainous areas, while several schools, beaches, national parks and ferry services were closed across the island.

[58] Kaohsiung officials urged residents to be vigilant regarding the storm, recalling the devastation caused by Typhoon Thelma in 1977, which severely impacted the city.

[68] The United States government, through the US Marines,[69] provided emergency aid and air transport support in response to the devastation caused by Krathon, particularly in Batanes.

[73] The Philippine Air Force mobilized its PZL W-3 Sokół helicopter to provide emergency supplies and personnel as part of the government's continued relief efforts for the typhoon-affected areas in Batanes.

[78][79] As of October 18, 2024[update], the National Disaster Risk Reduction and Management Council reported that a total of 380,778 people were affected,[80] with 11 displaced from their homes.

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
Krathon off the northeastern coast of Luzon on September 30
CWA radar imagery of Krathon tracking over the Balintang Channel (passing close to Sabtang, Batanes) before eventually making landfall over the southwestern coast of Taiwan
President Lai Ching-te inspected the Central Disaster Response Center and held a video conference with Pingtung County Mayor Chou Chun-mi
The Bell Boeing V-22 Osprey from the 15th Marine Expeditionary Unit landed at Basco Airport on October 8
Krathon passed directly near Sabtang in Batanes on September 30
A convenience shop was severely damaged during Typhoon Krathon