Garmin G500 Pilots Guide - Page 194

Radar Signal Reflectivity

Page 194 highlights

Foreword System Sec 1 PFD Sec 2 Attenuation can also be due to poor maintenance or degradation of the radome. Even the smallest amount of wear and tear, pitting, and pinholes on the radome surface can cause damage and system inefficiency. 4.8.2 Radar Signal Reflectivity 4.8.2.1 Precipitation Precipitation or objects more dense than water, such as earth or solid structures, will be detected by the weather radar. The weather radar will not detect clouds, thunderstorms or turbulence directly. It detects precipitation associated with clouds, thunderstorms, and turbulence. The best radar signal reflectors are raindrops, wet snow or wet hail. The larger the raindrop the better it reflects. The size of the precipitation droplet is the most important factor in radar reflectivity. Because large drops in a small concentrated area are characteristic of a severe thunderstorm, the radar displays the storm as a strong return. Ice, dry snow, and dry hail have low reflective levels and often will not be displayed by the radar. A cloud that contains only small raindrops, such as fog or drizzle, will not reflect enough radar energy to produce a measurable target return. MFD Sec 3 Features Avoidance Hazard Sec 4 Additional Sec 5 & Alerts Annun. Sec 6 Symbols Sec 7 Appendix A Glossary Sec 8 Index Appendix B Figure 4-57 Precipitation Type and Reflectivity 4-66 Garmin G500 Pilot's Guide 190-01102-02 Rev. B

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4-66
Garmin G500 Pilot’s Guide
190-01102-02
Rev. B
Foreword
Sec 1
System
Sec 2
PFD
Sec 3
MFD
Sec 4
Hazard
Avoidance
Sec 5
Additional
Features
Sec 6
Annun.
& Alerts
Sec 7
Symbols
Sec 8
Glossary
Appendix A
Appendix B
Index
Attenuation can also be due to poor maintenance or degradation of the
radome. Even the smallest amount of wear and tear, pitting, and pinholes on the
radome surface can cause damage and system inefficiency.
4.8.2
Radar Signal Reflectivity
4.8.2.1
Precipitation
Precipitation or objects more dense than water, such as earth or solid
structures, will be detected by the weather radar. The weather radar will not
detect clouds, thunderstorms or turbulence directly. It detects precipitation
associated with clouds, thunderstorms, and turbulence. The best radar signal
reflectors are raindrops, wet snow or wet hail. The larger the raindrop the
better it reflects. The size of the precipitation droplet is the most important
factor in radar reflectivity. Because large drops in a small concentrated area are
characteristic of a severe thunderstorm, the radar displays the storm as a strong
return. Ice, dry snow, and dry hail have low reflective levels and often will not
be displayed by the radar. A cloud that contains only small raindrops, such as
fog or drizzle, will not reflect enough radar energy to produce a measurable
target return.
Figure 4-57
Precipitation Type and Reflectivity