Clear air turbulence.
Clear air turbulence problems including forecasting inadequacy, detection device requirements, categories, etc
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Clear air turbulence problems including forecasting inadequacy, detection device requirements, categories, etc
Clear air turbulence simultaneously investigated by radar, jet aircraft, Jimspheres, and radiosondes
Clear air turbulence in stratosphere and troposphere
Clear air turbulence detection and warning by airborne devices including radar, IR spectrum, air temperature probes, ozone detection, etc
Clear air turbulence detection and warning by airborne devices including radar, IR spectrum, air temperature probes, ozone detection, etc
Clear air turbulence detection in troposphere by multifrequency radiometric sensor, noting multibeam system for supersonic aircraft
Simultaneous lower atmosphere clear air turbulence analysis by multiwavelength radar, jet aircraft and special rawinsondes
Sheer generated atmospheric clear air turbulence growth and dependence on atmospheric instabilities calculated numerically by invariant model
Detecting clear air turbulence using CO2 laser Doppler system
An airborne clear-air turbulence detector is being flight-tested on board NASA's C-141 and Learjet aircraft. The device is an infrared (IR) sensor in the water vapor band and is designed to detect changes in vapor concentrations associated with turbulence in shear conditions. Warnings of about 5 min have been demonstrated at flight altitudes from 9.1 to 13.7 km (30,000 to 45,000 ft). Encounter predictions were obtained 80% of the time, and false alarms were given about 6% of the time. Several simple algorithms were studied for use as signal output analyzers and for alert triggering.
A clear air turbulence (CAT) flight test to evaluate and test four different sensors in the detection and measuring of CAT and other meteorological targets that relate to turbulence is discussed. The primary types of CAT investigated were mountain wave CAT, jetstream CAT, CAT in cirrus clouds, and CAT in frontal wind shears, troughs, and ridges. The sensors included the CO2 pulsed Doppler lidar and three radiometers. One of the radiometers, at a frequency of 55.5 GHz, looked at atmospheric temperature structure. Another, at a frequency of 180.1 GHz, looked at atmospheric water vapor and investigated the feasibility of measuring at the microwave frequency the turbulence features seen in the infrared (IR) frequencies. An IR radiometer at 27 to 33 microns was the fourth sensor. This last device and the temperature structure radiometer worked well at all flight levels.
Radar detection of tropopause and clear air turbulence
Clear-air turbulence has become the largest single cause of weather-related injuries occurring in commercial carriers at cruising altitudes. A technique for objective operational CAT detection (the SCATR index) has been formulated. Its physical basis ties CAT to total energy dissipation as a response to meso- and synoptic-scale dynamical processes associated with upper-level jet stream/frontal zones. Early case studies using properly analyzed routine RAOB rawinsonde sounding data have shown promise.
Research on forecasting, detection, and incidents of clear air turbulence
The feasibility of detecting a thin cirrus and clear air turbulence from ERTS MSS data is explored. The result of analyses indicates that a thin cirrus not shown in conventional meteorological satellite picture can be revealed in ERTS MSS picture. It is also found that the core of jet stream can be located with high accuracy from ERTS pictures and the possible area of clear air turbulence can be predicted if the data of the quality of ERTS data are available in real time.
Occurrence frequency and intensity of clear air turbulence as function of altitude between 20,000 and 75,000 ft
Occurrence frequency and intensity of clear air turbulence as function of altitude between 20,000 and 75,000 ft