Page 273 - NS-2 Textbook
P. 273

268                                                                                     NAUTICAL SCIENCES












                                    COLD FRONTAL SURFACE



                                                                            COLD AIR
                                        COLDEST AIR
                                                                ! l':It---O(:CLUDED FRONTAL SURFACE


















                                           COLD AIR



                                                                               COLDEST  AIR


                                                        WARM-FRONT  OCCLUSION
          Two types of occluded fronts.  In  the  upper  drawing  of a cold-front occlusion, the cold  air  behind the (old front  is  colder than the cold  air
          ahead of the warm front,  pushing the warm front aloft. In  the warm-front occlusion on the bottom, the cold air ahead of the warm front is
          colder than the cold air  behind the cold front,  forcing the cold front aloft. From  Kotsch Weather for the Mariner,  133



          friction, these downdrafts take the place of updrafts and   A  thunderstorm  is  most  turbulent  in  the  area  of
          spread  out.  The entire  lower portion  of  the  cloud  be-  heaviest precipitation. Icing will often occur just above
          comes downdraft, and the high winds in the upper alti-  the freezing level, making this a very hazardous area for
          tudes  flatten  the  top  of  the  cloud into an anvil  shape.   an"craft.
          Rain is now falling heavily on the ground, but the storm   The  leading  gust of wind,  sometimes  called  a  mi-
          will dissipate in a short time.                        croburst, is one of a thtmderstorm's dangers. This gust oc-
                                                                 curs just prior to  the  passage of the  storm.  The  strong
                                                                 winds  at  the  surface  are  the  result  of  the  horizontal
                   WEATHER PHENOMENA WITH
                                                                 spreading-out of the storm's downdraft currents as they
                         THUNDERSTORMS
                                                                 approach the surface of the Earth. The speed of the first
          Rain is found in every thunderstorm. Some of this rain   gust usually is the highest recorded during any thunder-
          will form in regions below freezing level. Hail will form   storm and can blow in any direction--€ven in opposition
          if the updrafts carry melted or partially melted raindrops   to the sm-face wind that is "pushing" the storm. Such con-
          into the higher,  colder  altitudes.  Snow and  ice  crystals   ditions can result in u,vind shear/' "which is very danger-
          also  may be  in  any  thunderstornl,  ·winter  or  sumnlel~   ous to aircraft in the process of taking off or landing.
          though in summer they will fileH into rain vvhen nearing   Surging air currents in the thunderhead cloud create
          the Earth.                                             static electricity,  the  source  of  lightning.  This process is
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