Airborne weather radar
Navigation · Chapter 42 · DGCA CPL and ATPL
Why 3 cm, reading the colours and hail shapes, beams and modes, cloud tops by tilt, and flying round storms.
Remember
- 9 375 MHz (3.2 cm): big drops and wet hail; not fog, not CAT.
- Stabilised antenna; pencil beam for weather, fan (cosecant²) for short-range mapping.
- Green 12 mm/h, magenta turbulence; steep gradient and hooks = danger.
- Cloud top above you ≈ (tilt − ½ beam) × range × 100 ft. Beware shadow areas.
- STANDBY on the ground until the area is clear; WEA has swept gain, MAP/MAN manual gain.
What does a weather radar do, and what is it made of?
Eyes for storms
- What it is for • AWR (airborne weather radar) shows where the heavy rain is ahead, and so where the turbulence is • Also: cloud-top heights (using the tilt), a map of the ground below, and a range and bearing fix off a landmark
- The parts • A transmitter-receiver, an antenna in the nose, a display and a control box • The antenna is stabilised in pitch and roll: it stays level with the horizon while the aircraft climbs or banks
- Primary radar • It is a primary radar: the echo time gives the range • The sweep gives the bearing relative to the nose; range and bearing lines are drawn on the screen
- What the beam touches • Drag the tilt. The bright ring is where the beam meets the storm • On the wet core: red. On the dry ice top: almost nothing. Above it: nothing at all, though the storm is still there
Why 9 375 MHz, and why does the beam width matter?
Why 3 cm, why a narrow beam
- Match the drops • Echoes are strongest from things about as big as the wave. The drops that mean turbulence, big rain and wet hail, are about 3 cm • So the radar works on 9 375 MHz (X band): 300 ÷ 9 375 = 3.2 cm
- Not shorter, not longer • Move the wavelength. Shorter: every small droplet answers (clutter) · longer: the wave rolls past even the hail • Fog, stratus and clear-air turbulence (CAT) have no big drops: not shown
- Beam width • The beam is a 3–5° pencil, so it gets wider the further it goes • Far away it is wider than the gap between two storms: they paint as one. Closer, they split • A narrower beam needs a bigger dish: no room in the nose
- Water and ice on the radome • Water in the radome (the nose cover) or ice on it soaks up the energy, like food in a microwave oven • Echoes come back weaker, so storms look milder than they are
What do the colours mean, and where is the turbulence?
Reading the picture
This lesson is part of the Navigation plan. See plans
Which beam for weather, which for the ground, and what do the switches do?
Beams and modes
This lesson is part of the Navigation plan. See plans
How do you use the tilt, and find a cloud top?
Tilt and cloud height
This lesson is part of the Navigation plan. See plans
How do you use the radar to keep out of a thunderstorm?
Flying round storms
This lesson is part of the Navigation plan. See plans
How does it map the ground, and how do you use it safely?
Mapping and checks
This lesson is part of the Navigation plan. See plans
Test yourself on chapter 42
Test yourself
This lesson is part of the Navigation plan. See plans