PRIMUSr 880 Digital Weather Radar System
DConvective thunderstorms become much less reflective above the freezing level. This reflectivity decreases gradually over the first 5000 to 10,000 feet above the freezing level, as shown in figure 5- 10.
FREEZING LEVEL
AD- 35696@
Convective Thunderstorms
Figure 5- 10
The aircraft in figure 5- 10 has a clear radar indication of the thunderstorm, probably with a shadow in the ground returns behind it.
DIf the tilt angle shown in figure 5- 11 is not altered, the thunderstorm appears to weaken as the aircraft approaches it.
FREEZING LEVEL
AD- 35697@
Unaltered Tilt
Figure 5- 11
Radar Facts | A28- 1146- 102- 00 |
|