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Cases › NYC02LA088 · Part 121 airline

Boeing 767-224

Atlantic Ocean · 2002-04-22·N68160

0
fatal
1
serious
Serious injury
highest injury
—
damage

What happened

NTSB summary, verbatim

The airplane was in cruise flight at flight level 360, over the Atlantic Ocean, about 75 miles north of San Juan, Puerto Rico, when it encountered turbulence. One flight attendant sustained a serious injury, and one flight attendant and one passenger sustained minor injuries. The flight continued to its destination and landed without further incident. Review of National Weather Service Weather Surveillance Radar revealed echoes along the airway where the turbulence event occurred; which implied that the turbulent event was likely associated with a Convective Induced Turbulence (CIT) encounter related to the airflow associated with cumulonimbus activity, and possibly above and downwind of the cumulonimbus cloud tops.

Photographs

1the aircraft, and what the investigators found
The aircraft before the accident
242aq - Continental Airlines Boeing 767-224ER, N68160@ZRH,17.06.2003 - Flickr - Aero Icarus
Aero Icarus from Zürich, Switzerland · CC BY-SA 2.0 · Wikimedia Commons

Probable cause

the Board's determination
The airplane's inadvertent encounter which clear air turbulence during cruise flight.

Sequence of events

1 timed eventsfrom the FDR factual report · claude-sonnet-5
  1. 0230 ESTcruise flight over the Atlantic Ocean, about 75 miles north of San Juan, Puerto Ricop.1
    Aircraft encountered turbulence while in cruise flight

NTSB analysis

from the final report

The airplane was in cruise flight at flight level 360, over the Atlantic Ocean, about 75 miles north of San Juan, Puerto Rico, when it encountered turbulence. One flight attendant sustained a serious injury, and one flight attendant and one passenger sustained minor injuries. The flight continued to its destination and landed without further incident. Review of National Weather Service Weather Surveillance Radar revealed echoes along the airway where the turbulence event occurred; which implied that the turbulent event was likely associated with a Convective Induced Turbulence (CIT) encounter related to the airflow associated with cumulonimbus activity, and possibly above and downwind of the cumulonimbus cloud tops.