190-01895-00 Rev. A
Garmin G1000 Pilot’s Guide for the Diamond DA62
359
HAZARD AVOIDANCE
SY
STEM
O
VER
VIEW
FLIGHT
INSTRUMENTS
EIS
AUDIO P
ANEL
& CNS
FLIGHT
MANA
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HAZARD
AV
OID
ANCE
AFCS
ADDITIONAL
FEA
TURES
APPENDICES
INDEX
In areas of multiple heavy cells, use the Vertical Scan feature along with antenna tilt management to
examine the areas. Remember to avoid shadowed areas behind targets.
Figure 6-104 The Blind Alley
The Blind Alley at Close Range
The Large Storm Behind
t
oRnaDoes
There are no conclusive radar target return characteristics which identify a tornado. However, tornadoes
may be present if the following characteristics are observed:
• A narrow, finger-like portion extends and in a short time curls into a hook and closes on itself.
• A hook, which may be in the general shape of the numeral 6 (9 in the southern hemisphere), especially
if bright and projecting from the southwest quadrant (northeast quadrant in the southern hemisphere) of
a major thunderstorm.
• V-shaped notches.
• Doughnut shapes.
These shapes do not always indicate tornadoes, and tornado returns are not limited to these characteristics.
Confirmed radar observations of tornadoes most often have not shown shapes different from those of a
normal thunderstorm display.
h
ail
Hail results from updrafts carrying water high enough to freeze. Therefore, the higher the top of a
thunderstorm, the greater the probability that it contains hail. Vertically scanning the target return can
give the radar top of a thunderstorm that contains hail. Radar top is the top of a storm cell as detected by
radar. It is not the actual top, or true top of the storm. The actual top of a storm cell is seen with the eyes
in clear air and may be much higher than the radar top. The actual top does not indicate the top of the
hazardous area.
Hail can fall below the minimum reflectivity threshold for radar detection. It can have a film of water on
its surface, making its reflective characteristics similar to a very large water droplet. Because of this film of
water, and because hail stones usually are larger than water droplets, thunderstorms with large amounts
of wet hail return stronger signals than those with rain. Some hail shafts are extremely narrow (100 yards
or less) and make poor radar targets. In the upper regions of a cell where ice particles are dry (no liquid
coating), target returns are less intense.
