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Typhoon Sally (1964)

Pacific typhoon in 1964

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Through Atmospheric pressure, Pascal (unit) and China

Sally's winds lessened thereafter as it brushed the northern Philippines, buffeting areas north of Manila with strong winds and heavy rain and causing serious damage. A person drowned from the typhoon's onslaught, while the naval station at San Vicente and the adjoining village sustained an estimated $500,000 in damage. After crossing the South China Sea, Sally made landfall on the South China coast east of Hong Kong on September 10. Due to fears of a repeat of Typhoon Ruby, which struck the region less than a week prior, 10,000 people were evacuated ahead of the storm. Sally produced wind gusts as strong as 154 km/h (96 mph) and dropped torrential rain that damaged homes and crops and induced one landslide that killed nine people. However, the overall impacts in Hong Kong were less than forecast. Sally weakened as it moved into inland China and dissipated on September 11. The remnants of Sally moved northeast and contributed to severe flooding around Seoul, South Korea, leaving 211 people dead or missing and 317 people injured, though 206 people remain unaccounted for. Over 36,000 people were left homeless as over 9,000 homes were either destroyed or flooded, resulting in $750,000 in property damage. The floods were the region's most significant in two decades.

Meteorological history

The origins of Sally can be traced to the interaction of a trough of low pressure with a westward-propagating tropical wave. This led to the development of a vortex over the Marshall Islands on September 2. The next day, observations from ships in the region indicated that the system organized into a tropical depression approximately 240 km (150 mi) southwest of Eniwetok Atoll. Aircraft reconnaissance investigating the nascent cyclone later that day determined that Sally reached tropical storm strength while located roughly 320 km (200 mi) northeast of Chuuk State. During this time, Sally took a west-northwest course that would continue for the remainder of its duration. The storm intensified into a typhoon early on September 4. The next day, the center of Sally moved across southern Guam with a forward speed of 37 km/h (23 mph); one-minute maximum sustained winds near the center were estimated by the Joint Typhoon Warning Center (JTWC) to have reached 155 km/h (96 mph) during its passage of Guam.

Sally strengthened further as it traversed the Philippine Sea, and at 06:00 UTC on September 7, the JTWC analyzed Sally's one-minute sustained winds to have reached 315 km/h (196 mph); surface winds as fast as 370 km/h (230 mph) were estimated by aircraft reconnaissance probing the typhoon. The Japan Meteorological Agency (JMA) estimated that Sally's central barometric pressure decreased to 895 hPa (mbar; 26.43 inHg). This made Sally the strongest typhoon of the 1964 Pacific typhoon season as measured by both wind speed (tied with Opal) and central pressure. These winds were also among the fastest ever analyzed for a tropical cyclone globally. The center of Sally then moved near the northern Philippines, passing 40 km (25 mi) north of Aparri on September 9. The JTWC estimated that Sally's one-minute sustained winds decreased during this period, and continued to diminish further as the typhoon tracked across the South China Sea. At 15:00 UTC on September 10, Sally made landfall on the People's Republic of China east of Hong Kong with one-minute sustained winds of 155 km/h (96 mph). After moving inland, the system rapidly weakened, degenerating into a tropical storm later on September 10 and losing its identity as a tropical cyclone the following day over South China. The remnants of Sally continued towards South Korea and Japan before they were last noted on September 16 over southern Kamchatka.

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