JPATS Weather - NETC
JPATS Weather - NETC
JPATS Weather - NETC
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<strong>JPATS</strong> AVIATION WEATHER BOOKLET<br />
Figure 3-13 — Stationary Front<br />
Stationary Fronts<br />
Sometimes the frontal border between the air masses shows little or no movement. Since neither<br />
air mass is replacing the other, the front is called a stationary front (Figure 3-13). Stationary<br />
fronts are indicated on surface charts by an alternating warm and cold front symbols, retaining<br />
their original red and blue colors, but pointing in opposite directions. Even though the front may<br />
not be moving, winds can still be blowing. Surface winds tend to blow parallel on both sides of<br />
the front rather than against and or away from it. Therefore, a stationary front has a 180° wind<br />
shift. The wind shift may be from any one direction to the opposite direction, as stationary fronts<br />
are less likely to be aligned in any one particular direction.<br />
The weather conditions occurring with a stationary front are similar to those found with the<br />
warm front, but are usually less intense. The weather pattern of a stationary front may persist in<br />
one area for several days, until other, stronger weather systems are able to push the stationary<br />
front weather along its way.<br />
OCCLUDED FRONTS<br />
Occluded fronts form when a faster moving cold front overtakes a slower moving warm front.<br />
There are two types of occluded fronts, cold and warm. The type of occlusion that forms depends<br />
on which front remains in contact with the ground. For example, if the cold front remains in<br />
contact with the ground, then it is named a cold front occlusion.<br />
Occlusions are shown on surface charts with both cold and warm frontal symbols pointing in the<br />
same direction, but colored purple. Both types of occlusions tend to be aligned from NW to SE,<br />
and hence move toward the NE at the speed of the front that remains on the ground. The wind<br />
shift across either type of occlusion will be a 180° shift, as there are actually two fronts in the<br />
same location. Therefore, ahead of the occlusion, the winds will be the same as those ahead of<br />
the warm front, and behind the occlusion, the wind will be from the same direction as behind the<br />
cold front: the wind shift is SE to NW. Because the occluded front is the result of the meeting of<br />
3-14 Version 3.2/Dec 08