Bauer v. United States

289 F. Supp. 2d 944, 2002 U.S. Dist. LEXIS 26732, 2002 WL 32254571
CourtDistrict Court, N.D. Illinois
DecidedOctober 10, 2002
Docket00 C 8075
StatusPublished
Cited by4 cases

This text of 289 F. Supp. 2d 944 (Bauer v. United States) is published on Counsel Stack Legal Research, covering District Court, N.D. Illinois primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Bauer v. United States, 289 F. Supp. 2d 944, 2002 U.S. Dist. LEXIS 26732, 2002 WL 32254571 (N.D. Ill. 2002).

Opinion

FINDINGS OF FACT

LEINENWEBER, District Judge.

1. This Federal Tort Claims Act case arises out of the death of three passengers, John H. Bauer, William H. Bauér III and Terry A. Spurgin, aboard a Beechcraft A-36 airplane bearing FAA registration No. N1812A, which crashed while en route from Louisville, Kentucky to Aurora, Illinois on March 20, 1998. The pilot was Daniel L. Sanders who is not a party to this suit. The executors of the estates of the three deceased passengers bring these cases. The plaintiffs allege that the United States, through the Federal Aviation Administration (the “FAA”), Flight Service Station (“FSS”) personnel, and Air Traffic Control (“ATC”) personnel committed numerous negligent acts and omissions which contributed to cause the deaths of the three passengers.

2. The plaintiffs contend that the FSS pre-flight weather briefing was inadequate; the ATCs at the Evansville Center failed to solicit pilot reports of inclement weather, and failed to pass on to Sanders the pilot reports that they had in fact *946 received; and that the ATC at Terre Haute, Jennifer Stahley, failed to provide information concerning the availability of the airport at Robinson and provided improper vectoring to Sanders which created confusion. The plaintiffs contend that all of the foregoing were proximate causes of the crash.

3. The United States contends that the cause of the air crash was pilot error. The pilot left Louisville en route to Aurora, Illinois in the face of weather reports and forecasts that he would be flying through icing conditions for virtually his entire route. The icing conditions that he encountered caused an ice buildup on the aircraft which in turn caused the crash. The United States contends that location of the crash shows that the pilot could not have made the VOR approach to either the Sullivan airport or the Robinson airport, so that any incorrect vectoring was not a proximate cause of the crash. Instead of proceeding northward, the pilot should have returned to Louisville as soon as he encountered icing.

4. The National Weather Service provides a wide variety of weather forecasts, observations and analytical products which it makes available to flight Service Stations. This information is obtained from radar and weather satellites. Advisories, called AIRMETS, are provided to general aviation to inform pilots of hazards and are issued from the Weather Center at Kansas City, Missouri, and can cover multi-state areas. Center Weather Advisories (“CWAs”), are locally issued (here Indianapolis) and cover much smaller areas. There are several types of AIRMETS, but the one in issue in this case is an AIRMET ZULU, which is an AIRMET reporting icing conditions. Both an AIRMET and a CWA are forecasts. Another source of weather information is a pilot report (“Pi-rep”). This consists of a weather observation by a pilot of actual conditions encountered. The Pirep usually consists of the observation, the type of aircraft, altitude, and the direction the plane is heading. Flight Service Stations are the primary source for obtaining pre-flight weather briefings and in-flight weather information. The latter are available on designated frequencies called Flight Watch. Prerecorded in-flight weather advisories, including the AIRMETS, are continuously broadcast on the Hazardous In-flight Weather Advisory Service (“HIWAS”) frequency. Both Flight Watch and HIWAS were available to Sanders.

5. To have icing conditions, there needs to be below-freezing air temperature and visible moisture, e.g., clouds. There are two types of icing that are relevant to aviation: rime icing and clear icing. Rime icing is caused by freezing of micro droplets. When the droplets freeze, some air is trapped and the result is something similar to frost and can attach to the airplane. When water droplets are bigger than micro droplets, the drops hit the plane, lose their shape, run backwards and form clear ice. Freezing rain is caused by a temperature inversion whereby rain starts to fall in above freezing conditions, falls through an area that is below freezing, and freezes upon contact with the ground or, for example, an aircraft wing. “Mixed” is where there is a combination of rime and clear icing. Build up of icing, either rime, clear or mixed, tends to destabilize the plane.

6. During the late afternoon and early evening hours of March 20, 1998, a low pressure storm system was moving through the Ohio Valley. Precipitation in this region was mostly light snow and/or freezing rain or drizzle. As the low pressure system moved eastward there occurred a so-called “wraparound effect” of winds blowing counterclockwise, ie., generally from the north to the south behind *947 the low. This had the effect of decreasing temperatures in the southern portions of Indiana and Illinois. An AIRMET ZULU was issued at 5:00 P.M. EST, valid until 10:00 P.M. forecasting occasional moderate mixed/rime icing in clouds and precipitation between surface and 16,000 feet northeast of the Bradford-Cincinnati line and between 3,000 feet and 16,000 feet below, which included the area between Louisville and Indianapolis. Three pilot reports had been received at the Louisville FSS at Sandiford Airport, one from a Cessna 195 who reported light to moderate rime icing that was shed when he descended from 4,000 feet to 3,000 feet, another from a Cessna 340 who reported moderate to severe mixed icing at 6,000 feet, and one from an Aero Commander reporting light rime icing at 7,500 feet near Lafayette, Indiana. The surface weather conditions at Louisville at 6:56 P.M. were: Wind 220 degrees at 5 Knots; Visibility 10 miles; Sky Condition few clouds at 600 feet scattered, 2,700 feet overcast; and Temperature 7 C. Temperatures tend to get colder at higher altitudes except in the case of an inversion. It is estimated that the temperature at 4,000 feet was close to 0 C. The surface weather conditions at Terre Haute at 7:53 P.M. were: Wind 360 degrees at 11 Knots; Visibility 10 miles, light rain; Sky Condition overcast at 1,200 feet; and Temperature 1 C.

7. At approximately 6:18 P.M. on March 20, 1998, Sanders called the Louisville FSS by telephone indicating his intention to fly from Louisville to Aurora, Illinois, leaving about 30 minutes later. The pilot expressed concern about projected icing conditions. The briefing that was provided was as follows:

“Ok there is an AIRMET for occasional moderate rime or mixed icing along the entire route of flight ahm three thousand to sixteen thousand here locally up north it’s from the surface to sixteen thousand up there in the Aurora area and AIRMET for occasional I-F-R conditions along the entire route of flight. Turbulence at occasional moderate below eight thousand. That’s it on the flight precautions. Ahm low pressure currently located in get a hold of it here extreme eastern Kentucky. Its moving slowly to the east as it does it should pull some of the moisture with it but well what you’ll be encountering affecting your route of flight is the wrap around effect on that low pressure.”
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“Ok. Currently ... Sandiford reporting a ceiling of five hundred broken, two thousand eight hundred overcast. Ten miles surface wind two two zero at Seven and ah up through Terre Haute area they’re getting some snow there.

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Bluebook (online)
289 F. Supp. 2d 944, 2002 U.S. Dist. LEXIS 26732, 2002 WL 32254571, Counsel Stack Legal Research, https://law.counselstack.com/opinion/bauer-v-united-states-ilnd-2002.