JPATS Weather - NETC
JPATS Weather - NETC
JPATS Weather - NETC
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
<strong>JPATS</strong> AVIATION WEATHER BOOKLET<br />
relative humidity of the air. Cold air masses will usually have lower dew point temperatures than<br />
warm air masses. Higher dew points indicate a greater amount of moisture available to produce<br />
clouds, fog, or precipitation.<br />
Pressures<br />
Figure 3-5 — Pressure Changes Across a Front<br />
All fronts are located in troughs of low pressure. The arrows in Figure 3-5 indicate the trough<br />
(where low pressure extends outward from the center of the low), as well as the direction of<br />
movement of the low-pressure system. Therefore, when a front approaches a station, or a pilot<br />
flies toward a front, the pressure decreases. Pressure then rises immediately following frontal<br />
passage. Figure 3-5 illustrates this pressure fall and rise with the time-sequence of the weather at<br />
station NSE. The earliest time is pictured in the upper right, when the pressure is 1011 mb, and<br />
the last point in time is at the lower left, with a pressure of 1007 mb. Because of this pressure<br />
change, it is extremely important to obtain a new altimeter setting when flying in the vicinity of a<br />
front.<br />
Figure 3-6 — Wind Shift Across a Cold Front<br />
Version 3.2/Dec 08 3-7