Garmin Pilatus PC_6 User's Guide Page 286

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Garmin G950 Pilot’s Guide for the Pilatus PC-6
190-00870-00 Rev. B
274
HAZARD AVOIDANCE
SYSTEM
OVERVIEW
FLIGHT
INSTRUMENTS
EIS
AUDIO PANEL
& CNS
FLIGHT
MANAGEMENT
HAZARD
AVOIDANCE
AFCS
ADDITIONAL
FEATURES
APPENDICESINDEX
PRINCIPLES OF PULSED AIRBORNE WEATHER RADAR
The term RADAR is an acronym for RAdio Detecting And Ranging. Pulsed radar locates targets by transmitting
a microwave pulse beam that, upon encountering a target, is reflected back to the radar receiver as a return
echo. The microwave pulses are focused and radiated by the antenna, with the most intense energy in the
center of the beam and decreasing intensity near the edge. The same antenna is used for both transmitting and
receiving. The returned signal is then processed and displayed on the G950 MFD.
Radar detection is a two-way process that requires 12.36 µs for the transmitted microwave pulses to travel
out and back for each nautical mile of target range. It takes 123.6 µs for a transmitted pulse to make the round
trip if a target is ten nautical miles away.
Airborne weather radar should be used to avoid severe weather, not for penetrating severe weather. The
decision to fly into an area of radar targets depends on target intensity, spacing between the targets, aircraft
capabilities, and pilot experience. Pulse type weather radar detects only precipitation, not clouds or turbulence.
The display may indicate clear areas between intense returns, but this does not necessarily mean it is safe to fly
between them. Only Doppler radar can detect turbulence.
Airborne weather radar has other capabilities beyond weather detection. It also has the ability to detect and
provide distance to cities, mountains, coastlines, rivers, lakes, and oceans.
NEXRAD AND AIRBORNE WEATHER RADAR
Both Airborne Weather Radar and NEXRAD measure weather reflectivity in decibels (dB). A decibel is a
logarithmic expression of the ratio of two quantities. Airborne Weather Radar measures the ratio of power
against the gain of the antenna, while NEXRAD measures the energy reflected back to the radar, or the radar
reflectivity ratio.
Both systems use colors to identify the different echo intensities, but the colors are not interchangeable.
Airborne color radar values used by Garmin Airborne Color Weather Radar should not be confused with
NEXRAD radar values.
ANTENNA BEAM ILLUMINATION
The radar beam is much like the beam of a spotlight. The further the beam travels, the wider it becomes.
The radar is only capable of seeing what is inside the boundaries of the beam. The figure below depicts
a radar beam’s characteristics. The figure illustrates vertical dimensions of the radar beam, although the
same holds true for the horizontal dimensions. In other words, the beam is as wide as it is tall. Note that
it is possible to miss areas of precipitation on the radar display because of the antenna tilt setting. With the
antenna tilt set to zero in this illustration, the beam overshoots the precipitation at 15 nautical miles.
Figure 6-1 Radar Beam from a 10 inch Antenna
80
Altitude (x1000 ft.)
Range (nautical miles)
Antenna at Zero Tilt
Half Power at Beam Sidelobes
18,000 ft.
18,000 ft.
Max Power at Beam Center
10°
0
30 0 45 60 75 90 15
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