1937 Hong Kong typhoon

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1937 Great Hong Kong Typhoon
Surface weather analysis of the typhoon on 1 September
Meteorological history
Formed24 August 1937 (1937-08-24)
Dissipated4 September 1937 (1937-09-04)
Typhoon
Highest winds185 km/h (115 mph)
Lowest pressure958 hPa (mbar); 28.29 inHg
Overall effects
FatalitiesAbout 13,000
Damage$0.30
Areas affected
IBTrACSEdit this at Wikidata
Part of the 1937 Pacific typhoon season

The 1937 Great Hong Kong Typhoon was one of the deadliest typhoons in Hong Kong history, with a death toll estimated between 11,000–13,000. Part of the 1937 Pacific typhoon season, the tropical cyclone originated on August 24 to the south of Guam, which proceeded generally to the west-northwest. On September 1, the storm entered the South China Sea, and early the next day, the typhoon passed just south of Hong Kong before making landfall in southern China. It weakened after moving ashore, dissipating on September 3.

The territory suffered at least 11,000 fatalities,[1] while nearby Macau lost 21 people.[2]

Background

Ahead of the typhoon, Victoria Harbour was described as "crowded" in newspapers, amid a naval blockade of eastern China amid the Second Sino-Japanese War.[3] Time described the harbor as seventh busiest in the world... always alive with yachts, junks, ferries, sampans, freighters, liners, men-of-war.[4] The Hong Kong Observatory (HKO) was established in 1883, and a year later, the agency warned the public of an approaching typhoon using a gun. The system was replaced with bomb detonations, beginning in 1907. A decade later, the HKO introduced a numbered warning system to the public, with no. 1 as standby. The highest rating, no. 10, meant the potential for typhoon conditions, or maximum sustained winds of at least 119 km/h (74 mph).[5]

Meteorological history

Map plotting the track of the typhoon

The origins of the typhoon were from a storm located 320 km (200 mi) south of Guam on August 24. The September 1937 issue of the Monthly Weather Review described that "there was little evidence of its potentialities", as the storm moved west-northwestward across the western Pacific Ocean. On August 28, the USS Ramapo encountered the storm, observing an barometric pressure of 1003 mbar (29.61 inHg), and sustained winds of 61 km/h (38 mph). The observations suggested that the storm passed just south of the ship, although the intensity of the system was unknown at that point. Around August 30, the storm turned more to the northwest, causing it to remain north and east of majority of the Philippines. On September 1, it went through the Balintang Channel, passing 48 km (30 mi) south of Basco, Batanes. A station there recorded a pressure of 986 mbar (29.102 inHg), as well as a force 12 on the Beaufort scale, indicating hurricane-force winds. Thereafter, the typhoon entered the South China Sea, passing just north of Pratas Island, where a pressure of 993 mbar (29.327 inHg) was recorded.[6][7]

As the typhoon moved across the northern portion of the South China Sea, it intensified rapidly as it moved toward the southern Chinese mainland. On September 2 around 21:00 UTC[nb 1] the typhoon made landfall just west of Hong Kong, after passing only 12 km (7 mi) south of the British colony. The lowest pressure recorded there was 958 mbar (28.298 inHg). The typhoon's exact intensity was unknown, as its squalls of winds surpassed the capacity of the anemometer, which was greater than 201 km/h (125 mph).[6][7][8] The observations suggested that the typhoon struck with winds equivalent to a Category 3 on the Saffir-Simpson scale, or sustained winds of at least 180 km/h (112 mph).[9] The typhoon continued inland and weakened, dissipating northwest of Macau on September 3.[6][7]

Preparations and impacts

Damaged train tracks in Hong Kong

Late on August 31, the HKO, then known as Royal Observatory Hong Kong, issued warning signal no. 1, or standby. On the next day, the warning signal was raised to no. 5, which meant that gale force winds were expected for the territory.[6] The issuance prompted larger vessels to leave harbor and seek shelter in nearby bays.[10] The HKO upgraded the warning further to no. 10, meaning that typhoon-force winds were expected, at 17:58 UTC on September 1 (1:58 a.m. September 2 local time). Twelve minutes later, officials fired typhoon bombs to warn the public.[6] This marked the last occasion that typhoon bombs were used.[5] The no. 10 warning signal was issued overnight, and less than two hours before the typhoon made its closest approach.[6] As a result, the typhoon's ferocity was largely unexpected.[8]

As it moved ashore southern China, the typhoon produced a variety of damaging effects. Wind gusts reached at least 241 km/h (150 mph) in Hong Kong, when the piston of the anemometer stopped and failed to record any higher measurements.[8] Private anemometers recorded winds as high as 264 kilometres per hour (164 mph).[10] The mean hourly wind average in the territory reached 109 km/h (68 mph).[6] Along the coast, the powerful typhoon increased tides, with waves estimated at 9.1 m (30 ft) in Tolo Harbour. The high water mark at Tai Po was estimated at 6.2 metres (20.5 ft).[8] During its passage, the typhoon also dropped heavy rainfall, totaling 128.4 mm (5.055 in).[6]

The powerful typhoon killed thousands of people in Hong Kong, with a death toll between 11,000–13,000. This accounted for roughly 1% of the territory's population of 1 million.[11][9] However, many of the bodies were washed away and never found, with roughly 500 corpses found in the days after the typhoon. Fishermen accounted for majority of the deceased, after the typhoon capsized 1,855 fishing boats, including houseboats, as well as 28 ships bound for the ocean. Other sailors were unaware of the approaching storm. High tides washed many boats ashore and broke other vessels from their moorings, including the Asama Maru, the Conte Verde, and the Van Heutsz. The steamer An Lee broke from its moorings and struck the HMS Suffolk, causing 12 people to jump ship, one of whom missed and drowned. The An Lee later hit the HMS Duchess. Twenty ships sent out SOS distress signals.[11][6][4][10]

In mainland Hong Kong, the typhoon swept away an entire village in Tai Po Market, resulting in an estimated 300 fatalities. About half of Sha Tau Kok was wrecked. Across Hong Kong, the storm damaged houses and factories while also resulting in power and telephone outages. The winds uprooted trees and knocked down branches. During the height of the storm, nine buildings caught fire and were destroyed, resulting in dozens of deaths, after the fire brigade faced difficulty reaching the area. The high winds tore through roofs, signs, and lampposts, littering the road with debris.[11][4][10] British officials estimated the total damage around HK$1 million (US$300,000.[4]

Aftermath

Floodwaters in Hong Kong

Police and other officials used rope to attempt rescuing people caught by the floods.[4] Following the storm, a cholera outbreak developed in Hong Kong amid stagnant floodwaters.[4]

In 1938, the HKO published a report assessing the costs of typhoon damage over the preceding ten years. The 1937 typhoon accounted for 38% of the costs over the ten-year period, with the repairs reaching about HK$586,000.[11][nb 2]

See also

Notes

  1. ^ Dates and times are listed in Coordinated Universal Time (UTC) unless otherwise stated.
  2. ^ Dates and times are listed in Coordinated Universal Time (UTC) unless otherwise stated.

References

  1. ^ Strzepek, Kenneth M., Smith, Joel B. [1995] (1995). As Climate Changes: International Impacts and Implications. Cambridge, Cambridge University Press. ISBN 0-521-46796-9.
  2. ^ "MACAO TYPHOON DAMAGE. MANY LIVES LOST ON SHORE. FISHING FLEETS SUFFER". The Hongkong Telegraph (page 4). 4 September 1937.
  3. ^ "Typhoon Hits Hongkong". Nebraska State Journal. Associated Press. 2 September 1937. p. 1. Retrieved 27 April 2024.
  4. ^ a b c d e f "Foreign News: Hong Kong Typhoon". Time. 13 September 1937. Archived from the original on 14 September 2010. Retrieved 27 April 2024.
  5. ^ a b W.H. Lui, T.C. Lee and C.M. Shun (January 2018). Evolution of the Tropical Cyclone Warning Systems in Hong Kong since 1884 (PDF) (Report). Technical Report No. 109. Hong Kong Observatory. Retrieved 26 April 2024.
  6. ^ a b c d e f g h i Reverend Bernard F. Doucette. "Typhoons and Depressions over the Far East, September 1937" (PDF). Monthly Weather Review. 65 (9). Retrieved 25 April 2024.
  7. ^ a b c "1937 Not Named (1937240N13136)". International Best Track Archive for Climate Stewardship. Retrieved 25 April 2024.
  8. ^ a b c d "Typhoon Wanda August 27 to September 2, 1962". Hong Kong Observatory. Retrieved 26 April 2024.
  9. ^ a b Guangqing Huang; Wyss Yim (2007). "Reconstruction of an 8,000-Year Record of Typhoons in the Pearl River Estuary, China" (PDF). Environmental Science. Retrieved 26 April 2024.
  10. ^ a b c d "Typhoon in Hongkong". The Mail. Adelaide, South Australia. 23 October 1937. p. 6. Retrieved 28 April 2024.
  11. ^ a b c d A Review of Natural Disasters of the Past (PDF) (Report). Hong Kong Observatory. Retrieved 26 April 2024.

External links

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