Page 59 - AFMAN 15-111, 12 MAR 2019
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AFMAN15-111  12 MARCH 2019                                                                  59



                   11.2.5.  Each layer is separated from other layers by a space. The sky cover for each layer
                   reported is encoded by using the appropriate reportable contraction. The report of clear skies
                   (CLR or SKC) is reported by itself. The abbreviations FEW, SCT, BKN and OVC will be
                   followed, without a space, by the height of the cloud layer. (T-0).

                   11.2.6.  A  partial  obscuration  will  be  encoded  with  the  reportable  layer  construction
                   corresponding to the amount of the sky that is obscured followed by the layer height. A surface-
                   based obscuration will have a layer height of 000. A remark will also be appended for any
                   surface-based obscurations. For example:  fog obscuring 2/8ths of the sky would be encoded
                   in the body of the report as FEW000 and clarified in the remarks as FG FEW000. (T-0).
               11.3.  Sky Condition Algorithms.   An FBWOS derives sky condition by detecting the frequency
               and height of clouds that move over the sensor over a continuously averaged period of 30 minutes.
               The data collected from the sensor is processed into coverage amount, height and variability of
               clouds.
                   11.3.1.  FBWOS sensors are capable of reproducing a sky condition report comparative to that
                   of a human  weather technician but may perform poorly in situations where clouds develop in
                   the vertical but have little horizontal movement (i.e. convective clouds either remain directly
                   over sensor and are over-reported or do not pass over the sensor and are under-reported). When
                   equipped with multiple ceilometers, the data from the discontinuity sensors are examined and
                   compared with the primary sensor to determine the requirement to report non-uniform ceiling
                   conditions IAW Attachment 3.

                   11.3.2.  FBWOSs report sky condition from 100ft up to a maximum of 25,000ft. Note: Some
                   systems may report heights exceeding 25,000ft.

               11.4.  Standards  and  Reporting.    Sky  condition  is  an  evaluation  of  all  obscurations/clouds
               making up layers at different heights and is reported in oktas (eighths) using a code form with
               appended  height  above  the  surface.  Sky  condition  is  reported  in  all  METAR  and  SPECI
               observations.

                   11.4.1.  Clouds and/or obscuring phenomena (not necessarily all of the same type) with bases
                   at approximately the same level constitute a layer. They may be either continuous or composed
                   of detached elements. A trace aloft is evaluated as 1/8th; however, a surface-based obscuring
                   phenomenon is only classified as a layer when it covers at least 1/8th of the sky. All layers are
                   treated as opaque.
                   11.4.2.  Heights of layers are reported using a three-digit value representing hundreds of feet
                   above the surface and are rounded to a reportable increment. Layer heights up to 5,000ft are
                   reported to the nearest 100 feet, layer heights between 5,000ft and 10,000ft are reported to the
                   nearest 500ft and layers above 10,000ft are reported to the nearest 1,000ft. When a value falls
                   halfway between two reportable increments, the lower value is reported.
                   11.4.3.  Sky cover is determined using the summation principle. This principle states that the
                   sky cover at any level is equal to the sky cover in all lower levels up to and including the layer
                   in question. In other words, no layer can be classified as less than the layers below it and no
                   total sky cover can be greater than 8/8ths. See Figure 11.1 for an example of the summation
                   principle.
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