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FORECASTING THE INTENSITY OF SURFACE PRESSURE SYSTEMS
INDICATIONS ALOFT FOR DEEPENING AND FILLING OF SURFACE LOWS

Aerographers Mate 1 & C
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Figure  3-7.-Illustration  of  secondary  cyclone  development  over  the  eastern  Pacific. retarded portion of the cold front, the original warm development,  the  new  secondary  wave  cyclone  is front associated with the primary cyclone tends to wash rapidly moving, but with no appreciable deepening as it out, or become masked in the more or less parallel flow moves along the front and few, if any, indications of between the returning cold air from the high to the east occluding  (fig.  3-7,  step  2).  As  this  new  low  moves and the original warm feeding current. In this stage of eastward  along  the  front,  the  pressure  gradients 3-9





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