Typhoon Wanda was one of the most intense tropical cyclones on record in Hong Kong. It was the 59th disturbance in the record-breaking 1962 Pacific typhoon season, forming in August east of the Philippines. Typhoon Wanda reached peak winds of 175 km/h in the South China Sea, and it made landfall on Hong Kong on September 1, producing gusts of 261 km/h which, in combination with a high storm surge, damaged thousands of huts and left 72,000 people homeless. Wanda left a total of 434 deaths, and it is estimated that an identical typhoon striking today would cause HK$2.6 billion in losses.
Meteorological history
The precursor disturbance to Typhoon Wanda was first observed on August 23 near Pohnpei in the Federated States of Micronesia. That day, a circulation formed in the interaction between the Mid-Pacific trough and an easterly wave, with energy from a surge in the Easterlies in the Southern Hemisphere. Initially winds were very weak, and it tracked west-northwestward while slowly gaining intensity. The official track from the Japan Meteorological Agency indicated the system first developed into a tropical cyclone on August 25, whereas the Joint Typhoon Warning Center initiated advisories two days later, after it was observed by the Hurricane Hunters. It was designated Tropical Depression 59 while located about 1120 km northeast of the Philippines. Throughout most of its duration, the cyclone maintained a general west-northwest track, although initial forecasts had a northward bias that anticipated a track into Taiwan. On August 28, reconnaissance aircraft reported winds of 75 km/h, or tropical storm status; as such, the JTWC named the system Wanda. Throughout the day, Wanda quickly intensified, with the pressure dropping to 992 mbar and the winds reaching 110 km/h by the end of the day. The next day, Wanda attained typhoon status, and on August 30 it traversed the Luzon Strait between the Philippines and Taiwan. By that time, the typhoon was about 1600 km wide, and the next day rainbands began affecting southeastern China and Hong Kong. While approaching southeastern China, Wanda reached its peak strength of with the JTWC estimating a minimum pressure of 949 mbar. The typhoon weakened slightly before making landfall on Hong Kong at 0000 UTC on September 1, with winds of 150 km/h. A combination of cold air and land interaction caused Wanda to weaken rapidly, and the JTWC discontinued advisories about 18 hours after Wanda moved ashore. According to the JMA track, the system turned southwest into the Gulf of Tonkin, intensifying slightly before shifting southeastward and dissipating over Hainan on September 4. Typhoon Wanda was fairly well-forecasted, compared to other storms during the year. The average forecast error for 24 hours was about 260 km, whereas for 48 hours, it was 415 km ; both values were less than the seasonal average.
Impact
During its passage of Hong Kong, Wanda produced 263 mm of rainfall. The typhoon moved ashore during the daily high tide, resulting in a storm surge of at least 5 m above normal, especially around Tolo Harbour, which caused widespread flooding and damaged or destroyed thousands of huts and houses in Sha Tin and Tai Po. The strong winds and waves blew fishing vessels from the water onto the streets. Maximum sustained winds were 145 km/h, while gusts reached 260 km/h, stronger than any previous typhoon on record. Additionally, the lowest pressure during its passage was 953.2 mbar, which was the lowest on record at the RHKO. Overall, the typhoon caused 434 deaths and left 72,000 people homeless. There was never a finalized damage total, although it was estimated in the millions of dollars. Over 2,000 boats in the colony were either wrecked or damaged. As damage was so severe in Hong Kong, there were little reports of impact elsewhere, although the storm did move across portions of southern China. The typhoon Wanda is routed in Hong Kong near Cheung Chau, most parts of Hong Kong was in the right side of it, so the strong wind blew the wave into Tolo Harbour made the sea level rose, therefore Sha Tin became the hardest hit. Since a large number of people settled in squatter huts on low-lying coastal areas or precarious slopes, and the fishermen who were lived in fishing boats, it caused the big casualty when the typhoon hit Hong Kong, some of survivor claimed that the huge waves instantly cover up, sweeping the squatter huts and the home is dumped in front of them. They had to run to the railway station in a higher sea level, but the flood was also deep in the knees. It is estimated that every 5 squatter huts had 1 was destroyed or damaged by the typhoon in Sha Tin, which is one of the gathering place of squatter huts in Hong Kong at that time, approximately 3,000 squatter huts damaged in total. The road was blocked by a large number of damaged squatter huts and needed the British army to help to rescue the residents and clean upthe road. The heavy flooding increased the hardness of the rescue and clean up, there were 869 acres of farm land were flooded with sea water, over 30 percents were in Sha Tin, almost 65 percents of the low lying farm in Sha Tin were still affected two months later. The shops and store were also heavily damaged by the flood, many goods from the store were drifting on the street and it was difficult for them to reopen in short term.
