JPATS Weather - NETC
JPATS Weather - NETC
JPATS Weather - NETC
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
<strong>JPATS</strong> AVIATION WEATHER BOOKLET<br />
JX105 - THUNDERSTORMS<br />
OVERVIEW<br />
Thunderstorms contain many of the most severe weather hazards. They are often accompanied<br />
by strong wind gusts, severe turbulence, lightning, heavy rain showers, severe icing, and possibly<br />
hail and tornadoes. As a result, thunderstorms should be avoided if possible.<br />
About 44,000 thunderstorms occur daily over the earth and pilots can expect to encounter one<br />
occasionally. In some tropical regions, thunderstorms occur year-round. In the mid-latitudes,<br />
they develop most frequently in spring, summer, and fall. This chapter presents hazards a pilot<br />
must consider when flying in the vicinity of, or actually entering, a thunderstorm. Being familiar<br />
with these factors will help you better understand what is going on both inside and outside the<br />
cockpit. Knowledge of thunderstorm characteristics and the application of tested procedures will<br />
help aircrews operate more safely near thunderstorms.<br />
REFERENCES<br />
AFH 11-203, <strong>Weather</strong> for Aircrews, Volume 1, Chapters 1, 3, and 4.<br />
THUNDERSTORM DEVELOPMENT<br />
The basic requirements for thunderstorm formation are moisture, unstable air, and some type of<br />
lifting action. Lifted air does not always result in thunderstorm activity. Air may be lifted to a<br />
point where the moisture condenses and clouds form, but these clouds may not grow<br />
significantly unless the air parcel reaches a point where it will continue to rise freely (recall the<br />
LFC from Chapter 2). The higher the moisture content, the easier the LFC is reached. One of the<br />
four lifting methods (from Chapter 2) is necessary to force warmer air from its lower level to the<br />
LFC, which is the trigger to starting the cumulus cloud through the thunderstorm life cycle. Once<br />
moist air is lifted in an unstable environment, the rapidly rising unstable air quickly forms<br />
towering cumulus and eventual cumulonimbus clouds. The degree of vertical cloud growth often<br />
indicates the potential severity of the thunderstorm.<br />
THUNDERSTORM WEATHER HAZARDS<br />
Thunderstorms are accompanied by some or all of the following hazards: extreme turbulence,<br />
hail, microbursts, severe icing, lightning, and tornadoes.<br />
Turbulence<br />
Severe turbulence is present in all thunderstorms. One of the major characteristics of every<br />
thunderstorm is updrafts and downdrafts that can occur near each other creating strong, vertical<br />
shear and turbulence. This turbulence can extend over 5000 feet above the cloud tops and down<br />
to the ground beneath the cloud base. It can damage an airframe and cause serious injury to<br />
passengers and crew.<br />
The first gust or gust front of an approaching thunderstorm is another form of turbulence that can<br />
cause a rapid and drastic change in the surface wind (Figure 5-1). An attempt to take off or land<br />
with an approaching thunderstorm nearby could have disastrous results. Gust fronts can travel 5<br />
to 20 miles from the thunderstorm.<br />
Version 3.2/Dec 08 5-1