miles ahead of the front. These clouds are all found inthe warm air. Generally, unless the cold air is unstableand descending currents are weak, there are few cloudsin the cold air behind the front. Showers andthunderstorms occur along and just ahead of the front.The ceiling is low only in the vicinity of the front.Visibility is poor during precipitation but improvesrapidly after the frontal passage.Upper Air CharacteristicsBecause of the sinking motion of the cold airbehind the front and the resultant adiabatic warming,the temperature change across the front is oftendestroyed or may even be reversed. A sounding taken inthe cold air immediately behind the surface frontindicates only one inversion and an increase in moisturethrough the inversion. Farther back of the front, adouble inversion structure is evident. The lowerinversion is caused by the subsidence effects in the coldair. This is sometimes confusing to the analyst becausethe subsidence inversion is usually more marked thanthe frontal inversion and may be mistaken for thefrontal inversion.In contrast to the slow-moving cold front, the windabove the fast-moving cold front exhibits only a slightbacking with height of about 20 degrees between 950and 400 mb; the wind direction is inclined toward thefront at an average angle of about 45 degrees. The windcomponents normal and parallel to the front increasewith height; the wind component normal to the frontexceeds the mean speed of the front at all levels abovethe lowest layers. On upper air charts, the isotherms areNOT parallel to the front. Instead they are at an angle ofabout 30 degrees to the front, usually crossing the coldfront near its junction with the associated warm front.SECONDARY COLD FRONTSSometimes there is a tendency for a trough of lowpressure to form to the rear of a cold front, and asecondary cold front may develop in this trough.Secondary cold fronts usually occur during outbreaksof very cold air behind the initial outbreak. Secondarycold fronts may follow in intervals of several hundredmiles to the rear of the rapidly moving front. When asecondary cold front forms, the primary front usuallytends to dissipate and the secondary front then becomesthe primary front. Secondary fronts usually do notoccur during the summer months because there is rarelyenough temperature discontinuity.COLD FRONTS ALOFTThere are two types of upper cold fronts. One is theupper cold front associated with the warm occlusionthat is discussed later in this unit. The other occursfrequently in the areas just east of mountains in winter.This cold front aloft is associated with mP air crossingthe mountains behind a cold front or behind a coldtrough aloft and a very cold layer of continental polarair lying next to the ground over the area east of themountains. The area east of the Rocky Mountains is onesuch area in the United States. When warm maritimetropical air has moved northward from the Gulf ofMexico and has been forced aloft by the cold cP air, andcool mP air flows over the mountains, it forces its wayunder the warm mT air aloft. The resulting front thenflows across the upper surface of the colder cP air justas if it were the surface of the ground. All frontalactivity in this case takes place above the top of the cPlayer. Figure 4-33 shows an example of this type offront and the synoptic structure. Weather from cold4-35FRONTALZONEAG5f0433WESTCOOLmPWARMmTcPVERY COLDROCKYMOUNTAINSEASTFigure 4-33.—Cold front aloft.
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