Thai Airways International Flight 601

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Thai Airways International Flight 601
Thai Airways International Sud Aviation Caravelle (OY-KRE) at Stockholm-Arlanda Airport.jpg
A Thai Airways International SUD-Aviation Caravelle similar to the one involved.
Accident
Date30 June 1967 (1967-06-30)
SummaryWeather, pilot error
SiteNear Kai Tak Airport, Hong Kong
22°18′07″N114°13′02″E / 22.3020°N 114.2173°E / 22.3020; 114.2173
Aircraft
Aircraft type Sud Aviation Caravelle III
Aircraft nameChiraprapa
Operator Thai Airways International
Registration HS-TGI
Flight origin Haneda Airport, Japan
1st stopover Songshan Airport, Taiwan
Last stopover Kai Tak Airport, Hong Kong
Destination Don Mueang Airport, Thailand
Occupants80
Passengers73
Crew7
Fatalities24
Injuries56
Survivors56

Thai Airways International Flight 601 was a Sud Aviation Caravelle that crashed into the sea on landing at the former Kai Tak Airport, Hong Kong, in a typhoon on Friday, 30 June 1967.

Contents

Accident

Thai Airways International Flight 601 took off from Taipei Songshan Airport (TSA/RCSS) on an hour-long flight to Kai Tak Airport. The Sud Aviation Caravelle (Registration: HS-TGI), which had made its first flight in 1960, had 80 people aboard: 73 passengers and 7 crew. With the plane on ILS approach to runway 31 at Kai Tak (HKG/VHHH), the Captain Viggo Thorsen age 43 and Co-pilot Sanit Khemanand aged 50 became occupied trying to make visual contact with the ground, and failed to notice that the aircraft had descended below the decision height of 415 feet (126 m). The crew made an abrupt heading change (while already 80 feet (24 m) below the glide slope), and then entered a high-speed descent. The aircraft undershot runway 31 and crashed into the sea, killing 24 passengers.

Kai Tak Airport in 1971, some four years after the crash of Flight 601. Hong Kong Kai Tak Airport 1971.jpg
Kai Tak Airport in 1971, some four years after the crash of Flight 601.

Probable cause

The probable cause of the accident was pilot error, specifically not noticing that the aircraft had descended below the glide slope. The presence of strong wind shear and downdrafts as a result of then-present Typhoon Anita was a probable contributing factor. However, at the time of the accident there were no means of detecting such weather phenomena. Further factors included:

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