04 Airborne Weather Radar Flashcards
The two main tasks of an airborne weather radar (AWR) system?
The two main tasks of an airborne weather radar (AWR) system are for the detection of adverse weather and for ground navigation.
Requirement for weather radar?
5,700kg and more then 9 seats
Frequency of AWR?
Modern AWR systems use wavelengths of approx. 3 cm transmitting pulses, which reflect best off wet hailstones.
X-Band - 9.345Ghz - SHF
Range of AWR?
160nm - 320nm.
However normally used at about 80nm
- 90 degrees L and R.
- 15 degrees up and down.
AWR Stabalisation?
Modern AWR systems are stabilised in pitch and roll using the aircraft’s attitude reference system.
AWR Beam shape?
The AWR system utilises a 3–5° cone shaped (pencil) beam for weather detection.
Beam shape for ground mapping?
Skyworx- Fan shaped beam, effective maximum range of 50Nm to 60NM
ATPLQ - A narrow conical beam is used for weather detection that is approximately 5º in beam width, called a pencil beam.
The AWR control panel has the following controls?
- off/on switch;
- function switch with WX, WX+Turbulance(T) and MAP modes;
- gain-control setting (auto/manual);
- tilt/auto tilt switch.
Gain control?
Sensitivity, the higher the gain, the more sensitve the radar.
The colours used on the AWR display, in order of increasing intensity of precipitation, are:
- Green. - Light returns 0.7-4mm/hr
- Amber. - medium returns 4-12mm/hr
- Red. - strong returns >12mm/hr
- Magenta. - turbulance due to rainfall intensity.
AWR on the ground?
AWR should be used with extreme caution on the ground, with the beam tilted up.
Ground mapping
Good and bad returns for ground mapping function?
Good returns - Mountains, cities and skyscrapers
Bad returns - calm seas, fine sand, flat terrain
Ground mapping
Hill shadowing?
Gives a false impression of radar shadowing areas as being water. Corrected by flying higher to reduce shadowing.
AWR Range?
An AWR display uses azimuth and range marker lines to indicate bearing and range to targets.
Pilot use of the AWR?
The tilt and gain functions can be used, together with the azimuth and range lines, to determine flight paths around thunderstorms, as well as the altitudes of weather systems and elevations of ground features.