JPATS Weather - NETC
JPATS Weather - NETC
JPATS Weather - NETC
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<strong>JPATS</strong> AVIATION WEATHER BOOKLET<br />
visibilities are generally visual meteorological conditions (VMC), but isolated instrument<br />
meteorological conditions (IMC) exist in heavy precipitation and near thunderstorms. Wider<br />
areas of IMC conditions can exist in winter due to snow showers.<br />
Turbulence — Many active cold fronts have turbulent cloud systems associated with them, but<br />
thunderstorms may not always be present. Even when there are no clouds, turbulence may still<br />
be a problem. As a rule, expect a rough flight in the vicinity of an active cold front, even when<br />
flying at a considerable altitude.<br />
Precipitation and icing conditions — Active cold fronts usually have a relatively narrow belt of<br />
precipitation, especially if the precipitation is showery. Icing may be severe in cumuliform<br />
clouds. Slow-moving cold fronts may have a broader area of precipitation and a greater threat of<br />
remaining in icing conditions for a longer period.<br />
Thunderstorms and squall lines — Severe weather is implied to exist in areas of reported<br />
thunderstorms. Chapter 4 will detail the hazards associated with thunderstorms.<br />
Squall Lines<br />
Figure 3-10 — Squall Line Formation<br />
A squall line is a line of violent thunderstorms. They are indicated on surface charts by a dashed,<br />
double-dotted purple line. They develop 50 to 300 miles ahead of the cold front and roughly<br />
parallel to it. They form when cold air downdrafts flowing ahead of a cold front lift additional<br />
warm, unstable air. The uplifted air develops its own updrafts and downdrafts and starts the<br />
thunderstorm development cycle (Figure 3-10). Sometimes, however, squall lines can be located<br />
nowhere near a cold front, possibly from the convergence of air flows at one location. Squall<br />
lines are usually the most intense during the late afternoon and early evening hours, just after<br />
maximum daytime heating.<br />
It is often impossible to fly through squall lines, even with radar, since the storms are extremely<br />
close to one another. Similar to cold fronts, Squall lines will also have a 90° wind shift from the<br />
SW to the NW.<br />
Version 3.2/Dec 08 3-11