CHESTER, CA, USA
N216PB
Cessna 172P
There were no witnesses to the accident. A passing motorist saw the tail of the aircraft sticking out of a lake and notified authorities. Crush lines on the recovered wreckage disclosed that it impacted the water right wing low with a pitch attitude in excess of 45 degrees nose down. No preimpact mechanical malfunctions or failures were identified. The pilot rented the airplane and flew 47 miles to the mountain resort airport, landed, met some of his future in-laws, and loaded three of them onboard for a local sightseeing trip around the lake. He obtained his fixed wing private certificate 2 weeks prior to the accident, and this was the first flight with passengers. During training, he had only 1 flight involving a high-density altitude airport, with the balance of his training conducted at airports with elevations less than 1,000 feet msl. The density altitude at the accident site was 5,400 feet. The lake is in an oval shaped mountain valley 25 miles long by 15 miles wide surrounded by mountains, which rise 3,000 to 4,000 above the water's surface. The town and the airport are at the northwest end of the lake. The town borders the airport to the north, and mature pine trees that are 50 to 60 feet in height surround the field and provide obstacles for an approach or departure on any runway but 16/34. The airport manager said that because of the terrain and obstacles, and the proximity of the noise sensitive town to the north, pilots typically land on runway 34 and takeoff on runway 16. While he could not be certain, the airport manager believes the airplane departed on runway 16. The location of the wreckage would be consistent with an upwind to crosswind turn point for runway 16. The aircraft was found in a takeoff and initial climb configuration. Based on the aircraft's recording hour meter and the stopped electric clock, the accident occurred in the initial climb from takeoff on runway 16. The performance data for the airplane establishes it would have climbed to between 400 and 500 feet agl as it reached the accident location. Using flight planning charts for the airplane, the elapsed time on the recording hour meter does not support a conclusion that the pilot completed a run-up or had any appreciable ground run time prior to the accident takeoff. Between 1500 and 1600, the airport's automatic weather observation station recorded winds from 289 degrees at 9 mph with peak gusts to 23 mph. The system only records the highest peak wind gust during the hour-long observation period; however, it does not record the time of the wind peak. Surface winds are affected by friction and Coriolis deflection, which will produce an average increase in wind speed of 10 mph at the boundary between the layer next to the surface and the free flow layer above, which is typically about 400 feet agl. Coriolis deflection will cause the wind direction to change clockwise at the boundary, with a typical direction change of 10 to 20 degrees. Katabatic wind effects in mountainous areas can result in a rapidly moving air mass, which if an inversion layer is present, may flow over the lower layer. Therefore, the takeoff roll on runway 16 would have been with a right quartering tailwind, which moved closer to a direct tailwind and increased in speed as the aircraft climbed through 400 feet. Considering the recorded peak wind speed, it is likely the aircraft encountered a rapid change in wind velocity by as much as 25 to 30 mph. The flaps-up stall speed at zero degrees of bank is 44 knots indicated airspeed (KIAS) and 47 KIAS with 30 degrees of bank angle. Normal initial climb segment airspeed is 74 KIAS at 5,000 feet msl.
HISTORY OF FLIGHT On April 28, 2000, between 1500 and 1620 hours Pacific daylight time, a Cessna 172P, N216PB, collided with the surface of Lake Alamanor near Chester, California. The airplane was operated by Pacific Flight Services of Chico, California, and was rented by the pilot for a personal flight. The aircraft was destroyed in the collision sequence and sank. The private pilot and his three passengers sustained fatal injuries. The airplane was being operated under 14 CFR Part 91 as a personal flight when the accident occurred. The flight is believed to have departed the Chester airport between 1500 and 1530 for a local sightseeing flight around the lake. Visual meteorological conditions prevailed and a flight plan was not filed for the flight. No witnesses to the accident were identified by either Safety Board investigators or investigating officers from the Pulmas County Sheriff/Coroner's Office. Investigation disclosed that the pilot rented the airplane from the operator and departed from the Chico airport about 1430 and flew to the Chester airport, a distance of 47 miles. At the Chester airport, the pilot met with his fiance, her grandparents, and her younger brother. According to the fiance and other family members, the pilot loaded his fiancee's grandparents and her younger brother onboard the airplane to go sightseeing around the lake while the fiance waited for the group to return. This was the pilot's first flight with passengers since obtaining his fixed wing private pilot certificate 14 days prior to the accident. The airport manager and owner of the local fixed base operation (FBO) on the field witnessed the group of people walk out to the accident airplane and get in. He said he was about 100 feet away from the airplane and he heard it start up and also heard the subsequent takeoff. He said that he owns a Cessna, and the engine sounded "typical" and normal. The airport manager said he is also an airframe and power plant mechanic with inspection authorization. While he did not note the exact time, he believes that the airplane took off somewhere between 1500 and 1530. The airport manager said that pilots typically land on runway 34 and depart using runway 16 so that they fly over the lake and not the noise sensitive town of Chester. He said he could not be 100 percent certain, but he believed the pilot departed on runway 16 out over the lake. Shortly after 1600, a motorist driving along the west shore of the lake observed the tail of an airplane sticking out of the water and went to the U.S. Forest Service ranger station across the street from the airport to report the sighting. According to Pulmas County Sheriff's office, the 911 emergency call from the U.S. Forest Service office reporting the aircraft wreckage sighting was logged at 1625. The location of the wreckage was plotted on a USGS survey map by the responding search and rescue personnel from the Pulmas County Sheriff's office. The location as plotted was later determined to be about 4,600 feet on a magnetic bearing of 132 degrees from the approach end of runway 34 (or the departure end of runway 16). The location is 0.4 miles east of the lake's north-south oriented western shoreline. According to the airport manager, the position of the wreckage would be consistent with either a upwind to crosswind turn point for runway 16, or, a base to final turn point for runway 34. PERSONNEL INFORMATION The pilot's personal flight records, the operator's records, and the Federal Aviation Administration (FAA) airman and medical records files were reviewed. He held a private pilot certificate with ratings for rotorcraft helicopters and single engine land airplanes. The rotorcraft helicopter rating was issued on August 1, 1999, and the airplane single engine land add-on rating was issued on April 14, 2000. The pilot's most recent third-class medical certificate was issued without limitations on September 1, 1998. According to the pilot's flight logbook he had 131 hours total time, with 68 hours in rotorcraft, and 63 hours in fixed wing airplanes. All of the fixed wing flight time was amassed in Cessna 172 aircraft between September 1999 and the accident. Over half of the flights, including the pilot's practical flight test, were listed in the accident airplane. Of the 63 fixed wing flight hours, 10 were recorded as pilot-in-command. No logbook entries were recorded between the pilot's fixed wing practical flight test on April 14 and the date of the accident. Based on the identifiers listed in the logbook for flight origin and destination points, the highest elevation airport used by the pilot was about 2,500 feet msl, and only one flight was recorded to that airport. The balance of the flight activity was conducted in the greater San Joaquin Valley of California at airport elevations below 1,000 feet msl. According to family members, the passenger in the right front seat did not have any prior aeronautical experience. No record of the individual was found during a review of the FAA airman and medical records database. AIRCRAFT INFORMATION The Cessna 172P, serial number 17274440, was manufactured in November 1980, and had accrued a total time in service of 9,005 hours. The most recent annual inspection was completed on February 4, 2000, 156 hours prior to the accident. In addition, a 100-hour inspection was accomplished on April 5, 2000, 58 hours prior to the mishap. A Lycoming O-320-D2J engine, serial number L-1046-39A, was the original Cessna factory installed engine in the airframe and had accumulated the same total time in service as the airframe. The engine had accrued 1,052 hours since the most recent major overhaul. Annual and 100-hour inspections were accomplished on the dates noted for the airframe. In addition, a 50-hour inspection was completed the day prior to the accident. Review of the operator's aircraft status sheet and maintenance department records disclosed that there were no unresolved discrepancies at the time the pilot rented the airplane. The operator's records revealed that the airplane was refueled on the morning of the accident with the addition of 15.1 gallons of 100LL aviation gasoline. The operator reported that the addition of the fuel topped the aircraft standard range tanks to capacity (43 gallons total, 21.5 in each tank). Another renter pilot flew the airplane for 1.2 hours before the accident pilot rented it; comparison of the recording hour meter reading at the accident site and on the operator's rental log sheet for the pilot's departure from Chico revealed that the accident pilot flew the airplane for a total of 0.6-hours. Using average fuel consumption rates in the airplane flight manual climb and cruise performance charts, investigators conservatively estimated that the airplane had about 20 gallons of fuel onboard at the time of departure from the Chester airport. The disposition of the fuel load between the two standard capacity wing tanks could not be determined. As noted above, the recording hour meter registered 0.6 hours from the time the pilot took the airplane at Chico. Using the performance charts in the Cessna Aircraft Information Manual for the airplane, the flight time from Chico to the Chester airport was computed (the charts are appended to this report). The performance charts include adjustment factors for the takeoff and climb variances from cruise. A climb to 6,000 feet was assumed in the computations, along with a cruise at 75 percent power, and an additional 6 minutes was factored in for the start and taxi at Chico, and the taxi in to parking at the Chester Airport. The total elapsed time thus derived was between 32 and 38 minutes, or, 0.6 hours on the recording hour meter. Weight and balance computations were made for the takeoff at Chester, and at a zero fuel condition. The airplane empty weight, total moment, and center of gravity were obtained from the operator's maintenance records. The takeoff condition used the previously estimated 20 gallons of fuel. The occupant weights and seating positions were obtained from the Pulmas County Coroner's office. The detailed computations are appended to this report. For the takeoff condition, the gross weight was 2,258 pounds and the center of gravity was 42.4-inches. For the zero fuel condition, the gross weight was 2,138 pounds, with a center of gravity at 42.1 inches. According to the weight and balance charts in the airplane's flight manual, the allowable center of gravity range for the determined weights was 37.86 inches to 47.3 inches. The maximum authorized gross weight is 2,400 pounds. According to Cessna Aircraft engineering documents, the control surface travel range for the elevator trim tab is 19 degrees tab down (nose up) and 22 degrees tab up (nose down). During examination of the control system following wreckage recovery from the lake, the elevator trim tab jackscrew actuator was found at a 13-degree tab down (nose up) position (See Tests and Research section of this narrative). At the request of Safety Board Investigators, Cessna Aircraft conducted a series of flight tests with a similarly equipped Cessna 172P. The tests were conducted at a weight and center of gravity location replicating the condition of the aircraft when it arrived at Chester and during the subsequent accident flight takeoff. A normal full-flap approach and landing was made following the procedures specified in the Aircraft Information Manual; the elevator trim tab was then measured and found to be 3.9 degrees tab down (nose up). A 13-degree tab down position was established on the ground and the cockpit indicator marked to be able to return to that setting while in flight. The power off trim speeds at zero flaps and at 10, 20, and 30 degrees of flap extension were then established. At zero flaps, power off, the trim speed was between 53 and 60 knots. With 10 degrees of flaps, power off, the trim speed was 53 to 56 knots. At 20 and at 30 degrees of flaps, power off, the trim speed was 53 to 58 knots. With flaps up and starting at liftoff airspeed, full power was applied; the test pilot terminated the procedure when the nose lifted above 40 degrees. Review of the Cessna Aircraft Information Manual for the Cessna 172P disclosed that the flaps up stall speed at zero degrees of bank is 44 knots indicated airspeed (KIAS) and 47 KIAS with 30 degrees of bank angle. Normal initial climb segment airspeed is 74 KIAS at 5,000 feet msl, with a 470-foot-per-minute climb rate. AIRPORT INFORMATION At an elevation of 4,500 feet mean sea level (msl), Lake Almanor is in an oval shaped mountain valley 25 miles long by 15 miles wide surrounded by mountains, which rise 3,000 to 4,000 above the water's surface. The valley's long axis is oriented on a northwest to southeast line. The town of Chester and the airport are at the northwest end of the lake. The town borders the airport to the north, and mature pine trees that are 50 to 60 feet in height, on average, surround the field. The airport is on the shore of the lake at an elevation of 4,528 feet msl, and it has two runways. The traffic pattern altitude is 5,528 feet msl. Composed of a gravel surface, runway 5/23 is 5,320 feet long by 120 feet wide. The departure end of runway 23 has obstacles consisting of trees, power lines, and a road. The departure end of runway 5 has trees for obstacles. A departure on runway 23 would be toward rising mountainous terrain, while a departure on runway 5 would be toward the lake's shoreline. Runway 16/34 is asphalt surfaced and is 5,000 feet long by 100 feet wide. The departure end of runway 34 has obstacles consisting of trees, power lines, and a road. The town of Chester is immediately north of the airport and a departure on runway 34 would be over the residential and business districts, and toward rising mountainous terrain. A departure on runway 16, or an arrival to runway 34, would be over the lake and without obstructions. Runway 34 has right-hand traffic. According to the airport manager, because of the surrounding terrain and obstacles, and the proximity of the noise sensitive town to the north, pilots typically land on runway 34 and takeoff on runway 16. METEOROLOGICAL INFORMATION The US Forest Service maintains an automatic weather observation station near the airport. The 1500 observation recorded a temperature of 56 degrees Fahrenheit, with 33 percent humidity, and winds from 273 degrees at 7 mph with peak winds at 18 mph. The 1600 observation recorded a temperature of 54 degrees Fahrenheit, with 35 percent humidity, and winds from 289 degrees at 9 mph with peak winds at 23 mph. The system only records the highest peak wind during the hour-long observation period; however, it does not record the time of the wind peak. Other wind speed transients between the steady state value and the highest peak value would not be recorded. Based on the recorded temperature and station pressure at the Forest Service observation unit, the density altitude was calculated to be about 5,400 feet during the probable time frame for the accident. The airport manager said the weather on the day of the accident was "breezy" with temperatures in the mid 50's. No unusual meteorological phenomena were observed in the vicinity of the lake, or reported by any pilot arriving at the airport on the day of the accident. The closest official aviation weather observation stations are: Red Bluff, California, 55 miles west of the site; Chico, 47 miles southwest; and Blue Canyon, California, 73 miles southeast. All of these stations are separated from Lake Almanor by one or more mountain ranges. During the probable time frame of the accident, the stations were reporting westerly winds below 12 knots. The upper air soundings from the Reno, Nevada, and Medford, Oregon, reporting stations were showing northwesterly wind flows at 15 knots or less below 10,000 feet. FAA Advisory Circular 00-6A, "Aviation Weather," and the textbook "Weather Elements," (Blair/Fite, 1975, Prentice-Hall, Inc., Englewood Cliffs, New Jersey) were reviewed regarding the effects of surface friction and Coriolis deflection on surface winds. According to both sources, protuberances in the surface induce a frictional slowing effect on wind velocity close to the surface; the rougher the surface (the more and larger the trees, buildings, etc.), the more pronounced the slowing effect. While the velocity change depends on many factors (including the terrain roughness, existence of a inversion layer, and the lapse rate of the atmosphere, among the most typical), the average velocity change is on the order of a 10 mph increase as you leave the frictionally affected layer. The boundary zone where the frictional effects rapidly decrease is usually in the 300- to 500-foot agl range. The Coriolis effect induces a change in the direction of the wind flow to the right (clockwise) in the northern hemisphere as you move away from the surface; at the boundary zone between the frictionally affected wind layer and the free air layer, the directional change is in the 10- to 20-degree range. Katabatic winds occur in mountainous areas and result from cold heavy air masses that flow down mountain slopes into valleys. As the Katabatic wind flow moves down a mountain slope, it is heated and dried, and will displace the warmer air masses in the valleys. If an inversion layer is present, the Katabatic wind may flow over the lower layer. WRECKAGE AND IMPACT The location of the wreckage was plotted on a USGS survey map by the responding search and rescue personnel. The location was later determined to be about 4,600 feet on a magnetic bearing of 132 degrees from the approach end of runway 34 (or the departure end of runway 16). The geographic coordinates of the airplane wreckage were west longitude 121 degrees 13.8 minutes by north latitude 40 degrees 15.8 minutes. As plotted on a USGS 7.5-minute chart, the approach end of runway 34 was west longitude 121 degrees 14.38 minutes by north latitude 40 degrees 16.56 minutes. According to the Pulmas County Sheriff's Office, two of the passengers (the fiancee's Grandparents) had a residence on the west
The pilot's encounter with a wind shear at low altitude, which resulted in a loss of control and a stall/spin. Factors in the accident were the high density altitude and the pilot's lack of experience and training in high density altitude operations. The pilot's decision to takeoff downwind, while reasonable given the nature of the obstacles and terrain on the other runways, set up a situation where decreased safety margins existed and is considered a factor.
Source: NTSB Aviation Accident Database
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