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               6. Isobars

               The pressure at each statton is marked on the weather map and lines called Isobars are drawn
               to  connect  the  points  of  equal  pressure.  Many  of  these  lines  make  complete  circles  and
               surround areas marked H (high) or L (1ow). Isobars are similar to the lines that are drawn on
               regular surface maps to show elevation. However, instead of indicating the elevation of terrain
               and the steepness of slopes, Isobars indicate the amount of pressure and steepness of pressure
               gradients. If the gradient (slope) is steep, the isobars will be close together, s and the wind will
               be strong. If the is gradual, the lsobars will be far apart, and the win light. Isobars provide useful
               information about the winds aloft. Close ith, wind direction is modified by the terrain over ses,
               and wind speed is reduced by friction with  The At tudes two or three thousand feet above the
               surface, however Is greater and the direction is  usually parallel to the isobars.








































                                                         Figure 4
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