NTSB CAROL · Event
Event LAX02LA146
Registry · N182UA
FAA Aircraft Registry record.
Make / Model
BOEING 747-422
Year of manufacture
1991 · 11 years old at event
Engine
P & W PW2040
Seats / Engines
495 seats · 4 engines
Last airworthiness date
19911024
ADS-B equipped
Yes — Mode-S A149DD
Registrant of record
UNITED AIRLINES INC
Source: FAA Aircraft Registry (releasable master file).
Aircraft involved
Probable cause & findings
An in-flight encounter with clear air turbulence and wind shear, which resulted in a serious injury to a flight attendant.
Factual narrative
On May 1, 2002, at 0629 coordinated universal time (UTC), a Boeing 747-422, N182UA, encountered clear air turbulence while climbing through approximately 31,000 feet and while in international airspace over the Pacific ocean about 700 miles north of New Zealand. According to the airplane's onboard Flight Management Computer (FMC) recorded data, the aircraft was at location 174.0027 degrees east longitude and 24.4684 degrees south latitude when the encounter occurred. The airline transport certificated pilot and remaining 3 flight crewmembers were not injured. Of the 17 flight attendant crewmembers, 1 was seriously injured, 1 received minor injuries, and 15 were not injured. Of the 269 passengers aboard, 5 received minor injuries and 264 were not injured. The airplane was not damaged. The flight was operated by United Airlines, Incorporated, under 14 CFR Part 121, as flight 862, a regularly scheduled international passenger flight. The flight departed from Sydney, Australia at 0353 UTC and was destined for San Francisco, California. Following the encounter with turbulence, the flight crew altered course and landed at Auckland, New Zealand at 1056 UTC. Visual meteorological conditions prevailed and the flight was operating on an instrument flight plan. According to the Captain, the airplane was flying over a flat broken cloud layer with a smooth ride. He said, "Passing 25 degrees south at FL310 we noticed that the cloud tops were gradually rising. Radar showed very little - a few green returns off to the right. We were in an area of no forecasted turbulence or cumulonimbus cloud buildups. I turned on the seatbelt sign and made a passenger announcement, as it appeared we would soon be just above or in the cloud tops and I expected a few light bumps although the clouds looked benign. After entering the top of the cloud layer...we encountered 10 - 15 seconds of sharp severe turbulence with momentary over speed warning and stick shaker." The captain said that he called the Purser and he was advised of flight attendant and passenger injuries. He contacted dispatch and was advised that he should divert to Auckland. After consulting with an onboard doctor and a company doctor in Chicago, the airplane diverted. According to one of the flight attendants, he was assigned the position number 4 at door 3 left outboard. He said, "About 3 to 3 1/2 hours into the flight, the seat belt sign was illuminated. As per my duties, I went to check seat belts. When I reached row 59 on the left side of the plane, the pilot announced that flight attendants should be seated. At that moment, I sat down immediately on the floor between seats 59b and 59d. I held on to the bar under seat 59b. Within seconds, the plane started to go through very, very, violent turbulence. It started to fish tale...What I saw however was something totally different. Two flight attendants had started counting the merchandise in the duty free carts." He said he saw one of attendants counting the duty free merchandise was thrown to the left of the airplane along with the duty free cart. The other flight attendant near to the duty free cart was also injured. The duty free cart ended up upside down, and all the merchandise was strewn over the floor. The seriously injured flight attendant was struck by the duty free cart. According to Digital Flight Data Recorder (DFDR) data, at 0628:58 a series of oscillating vertical and lateral accelerations began that lasted until 0630:38. The vertical accelerations (expressed in units of gravity or "g's", 1.0 is normal) ranged from a low of +0.31 to a high of +1.7. The lateral accelerations (a value of zero is normal) ranged from 0.119 left to 0.115 right. During the time frame of the encounter, the FMC reported winds went from 92 knots to 50, then back to 101. The indicated airspeed also varied from a pre-encounter average value of 315 knots to a peak of 344 before returning to the nominal 315 value. The investigation reviewed the dispatch and flight release package provided to the flight crew. The weather forecast portion of the document noted that in the vicinity of 173 degrees east and 25 degrees south the upper air winds between 31,000 and 35,000 feet were forecast to be from 290 degrees at 102 to 113 knots. The document also noted the possibility of moderate or lesser turbulence from longitudes 164 degrees east to 172 degrees east along the planned flight track. Two SIGMETS were listed on the documents. The first, SIGMET AMMC MW01 (valid from April 30 at 2200 UTC to May 1 at 0400 UTC) forecast severe clear air turbulence between 25,000 and 35,000 feet, though the area concerned was some 900 nautical miles south and west of the accident location. The second one, SIGMET NTAA NR01 (valid on May 1 from 0200 to 0800 UTC) forecast isolated and embedded cumulo nimbus clouds with tops to 46,000 feet over a wide area well west and north of the planned flight track. The National Weather Service Significant Weather Forecast Chart issued at 1700 UTC on April 30 and valid until 0600 UTC on May 1 showed a 120 knot jet stream and moderate or lesser clear air turbulence south of the accident location and an area of isolated cumulo nimbus clouds with tops to 40,000 feet to the north. No SIGMETS were in effect for turbulence. The flight encountered severe turbulence while operating at 31,000 feet msl, and a flight attendant sustained a serious injury. The encounter occurred near position 174 degrees 20 minutes east longitude and 24 degrees 18 minutes south latitude. According to the captain, prior to the turbulence event, the airplane was flying over a flat broken cloud layer with a smooth ride. He reported, in part: "Passing 25 degrees south at FL310 we noticed that the cloud tops were gradually rising. Radar showed very little - a few green returns off to the right. We were in an area of no forecasted turbulence or cumulonimbus buildups. I turned on the seatbelt sign and made a passenger announcement." The seriously injured flight attendant was in the process of securing the duty free cart when she was struck by it during the turbulence encounter. Digital Flight Data Recorder (DFDR) data showed that the airplane experienced a series of oscillating vertical and lateral accelerations that lasted almost 2 minutes. The vertical accelerations (expressed in units of gravity or "g's", 1.0 is normal) ranged from a low of +0.31 to a high of +1.7. The lateral accelerations (a value of zero is normal) ranged from 0.119 left to 0.115 right. During the time frame of the encounter, the airplane's Flight Management Computer reported winds aloft went from 92 knots to 50, then back to 101. The indicated airspeed also varied from a pre-encounter average value of 315 knots to a peak of 344 before returning to the nominal 315 value. Review of the weather portion of the dispatch and flight release package provided to the flight crew noted that in the vicinity of 173 degrees east and 25 degrees south the upper air winds between 31,000 and 35,000 feet were forecast to be from 290 degrees at 102 to 113 knots. The document also noted the possibility of turbulence from longitudes 164 degrees east to 172 degrees east along the planned flight track. The National Weather Service Significant Weather Forecast Chart valid for the flight showed a 120 knot jet stream and the possibility of occasional moderate or lesser clear air turbulence south of the accident location and an area of isolated cumulo nimbus clouds with tops to 40,000 feet to the north. The only SIGMETS in effect for turbulence concerned an area some 900 miles to the west and south of the accident location. Source: NTSB Aviation Accident Database (Pre-2008 Archive) Retrieved: 2026-02-12
Verbatim from NTSB's published report. Source file
NTSB_2002_LAX02LA146.txt.
Findings + structured fields enriched from FAA avall.mdb.
Full investigation docket on
data.ntsb.gov ↗.
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Related research
What the literature says.
Academic papers and agency reports matching this event's aircraft type or causal vocabulary (wind shear, turbulence). Sourced from NASA NTRS, NTSB Safety Studies, FAA CAMI, AOPA Air Safety Institute, Embry-Riddle Scholarly Commons, arXiv, and the Semantic Scholar academic graph.
- NASA NTRS 2019 · Contractor Report (CR)
An Examination of Aviation Accidents Associated with Turbulence, Wind Shear and Thunderstorm
The focal point of the study reported here was the definition and examination of turbulence, wind shear and thunderstorm in relation to aviation accidents.
- NASA NTRS 2019 · Preprint (Draft being sent to journal)
Convectively Induced Turbulence Encountered During NASA's Fall-2000 Flight Experiments
Aircraft encounters with atmospheric turbulence are a leading cause of in-flight injuries aboard commercial airliners and cost the airlines millions of dollars each year.
- NASA NTRS 2019 · Technical Memorandum (TM)
Some aspects of wind shear in the upper atmosphere
Hydrodynamic turbulence and wind shear in upper atmosphere
- Embry-Riddle Scholarly Commons 2019 · Journal article (IJAAA)
Low Level Turbulence Detection For Airports
Abstract—— Low level wind shear and turbulence present a serious safety risk to aircraft during the approach, landing and take-off phases.
- Embry-Riddle Scholarly Commons 2018 · Journal article (IJAAA)
Evaluating the Effect of Turbulence on Aircraft During Landing and Take-Off Phases
—— Low level wind shear and turbulence present a serious safety risk to aircraft during the approach, landing and take-off phases.
- arXiv 2026 · arXiv preprint
Direct Numerical Simulations of Ice-Ocean Boundary Turbulence
Turbulent heat and freshwater transport at ice-ocean interfaces controls glacier and iceberg melt rates, yet the underlying physics remains poorly constrained.
Browse the full corpus — academia portal ↗