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Ch-9 Weather TheoryV8-BAK_Basic Master Frame.qxd  12/19/2019  7:46 PM  Page 65






                                           Chapter 9 -  IFR Aviation Weather Theory                                       9-65

                     this category. This doesn’t mean, however, that airplanes  Years ago Project Rough Rider (and subsequent govern-
                     in the pre- ’69 category can’t withstand vertical gusts of  ment  studies)  established  a  correlation  between  the
                     greater intensity. This was just the minimum vertical gust  amount  of  water  suspended  in  a  cloud  and  the  vertical
                     requirement necessary according to the regulations at the  gusts found within that cloud (measured in feet per sec-
                     time.                                                  ond)  as  shown  in  Figure  113.  If  we  can  equate  rainfall
                       Now let’s talk about water.                          rates with radar reflectivity or dBZs, we can make some
                       As  you’ve  already  learned,  to  keep  large  volumes  of  interesting  assumptions  using  the  results  of  the  Rough
                     water suspended in the atmosphere it takes a lifting force,  Rider study.
                     otherwise known as updrafts. The more water suspended    It turns out that rainfall rates producing radar reflec-
                     within  a  cloud  the  greater  the  lifting  force  or  updraft  tivity  ranging  from  16  to  29  dBZs  (known  as  a  Level  1
                     that’s  required  to  keep  it  there.  When  the  amount  of  radar return) generate a 100% probability of light turbu-
                     water suspended exceeds the lifting force that suspends it,  lence and a 10% chance of moderate turbulence. Light tur-
                     the water falls. We call this rain and measure the amount  bulence  is  defined  as  vertical  gusts  from  0-19  FPS  and
                     in inches per hour.                                    moderate turbulence is defined as vertical gusts from 20
                       It doesn’t have to rain, however, for us to measure the  to 34 FPS.
                     amount of water suspended inside the cloud. We can mere-  Rainfall rates producing radar reflectivity ranging from
                     ly identify the amount of water in a cloud using radar and  30 to 39 dBZs (known as a Level 2 radar return) generate
                     say that if it did rain, then the rainfall rate would be a spe-  a 100% probability of light turbulence, a 40% chance of
                     cific amount, calibrated in inches per hour.           moderate  turbulence,  and  a  2%  chance  of  severe  turbu-
                       Given this observation, it’s logical to say that a cloud  lence. Severe turbulence is defined as vertical gusts from
                     with a rainfall rate (or potential rainfall rate) of .5 inches  35 to 49 FPS.
                     per hour has less updraft action than a cloud with a rain-  Rainfall rates producing radar reflectivity ranging from
                     fall rate of 2 inches per hour. We can conclude that the  40 to 49 dBZs (known as a Level 3 and 4 radar return) gen-
                     larger  the  rainfall  rate  (or  potential  rainfall  rate),  the  erate a 100% probability of light turbulence, a 90% chance
                     stronger the updrafts found inside a cloud.            of  moderate  turbulence,  a  10%  chance  of  severe  turbu-
                       As you undoubtedly know, radar energy is reflected by  lence,  and  a  3%  chance  of  destructive  turbulence.
                     solid objects, not clouds themselves. The water suspended  Destructive turbulence is defined as vertical gusts of 50
                     in a cloud is a solid object, but the cloud itself isn’t. The  FPS and higher.
                     more water suspended within the cloud, the greater the   Now you know the answer to the question, “What cri-
                     ratio of radar energy returned for a given amount sent out  terion  distinguishes  a  convectively  harmless  cumulus
                     by the radar unit. The amount of this reflected radar ener-  cloud from one that can damage an airplane?” The answer
                     gy, referred to as reflectivity or Z, is calibrated in the form  is:  Any  convective  cloud  with  a  radar  reflectivity  of  40
                     of a quantity known as dBZ or decibels of Z.           dBZs (a Level 3 radar return) or higher needs to be avoid-
                       Now things are about to get really interesting.      ed and treated as an immediate threat to your safety aloft.



                       Turbulence Probability
                        The turbulence probability
                       chart provides you with a
                       statistical means of estimat-
                       ing the probability of  turbu-
                       lence based on the amount
                       of water in a cloud.
                        For instance, if a cloud
                       has sufficient water to reflect
                       radar energy to a value of
                       40 to 49 dBZs, then there is
                       a 3% chance of destructive
                       turbulence (at the higher 49
                       dBZ value), a 10% chance
                       of severe turbulence (at the
                       higher 49 dBZ value), and a
                       100% chance of light
                       turbulence in that cloud.
                        Because of this potential
                       for severe and destructive
                       turbulence, pilots always
                       avoid cloud areas/masses
                       containing 40 dBZ and
                       higher.                                                                                         Fig. 113
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