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

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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

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Unaltered Tilt

Figure 5- 11

Radar Facts

A28- 1146- 102- 00

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Image 62
Honeywell 880 manual Convective Thunderstorms, Unaltered Tilt