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          Methodology
          and Algorithm  
        
         
      Algorithm
      Description 
      There are
      many methodologies used in forest fires detections. Some of them are very
      simple and basic; others are very complicated and involve complex issues.
      However, there are a limited number of methods that is commonly used. Most
      notable is the Kaufman algorithm, which has been developed to achieve more
      accurate measurements.
      A number of remote sensing systems, e.g., AVHRR, use this algorithm or a
      modified version of it. In the Kaufman algorithm, each and every pixel has
      to undergo 6 “tests.” When a pixel passes through all of the tests, we
      can call it a forest fire. For explanation purposes, we’re going to
      elaborate on these tests specifically in the content of AVHRR. However, it
      is crucial to understand that Kaufman algorithm is not solely limited for
      the use of AVHRR remotely sensored data. These tests are as follows:
      
       
      ·        
      Detection Test: Fires are detected when band 3 (3.7 micrometers) is saturated or very
      close to saturation by the income radiation from the fires. Band 3 is
      called saturated when the AVHRR sensor receives a thermal signal of around
      320 K.
      
       
      ·        
      Warm Background test: The temperature reading in band 3 should be greater
      than the reading band 14 (11 micrometers) plus 15 K. If a pixel makes this
      condition true, then it means that the background is not what saturates
      band 3.
      
       
      ·        
      High Reflective Cloud test: It is common for the clouds to have similar
      readings to those of fires. This is because clouds highly reflect solar
      energy radiation. Thus, we have to exclude any cloud cover from the data
      set. We can say for sure that there the reason for band 3 saturation is
      not cloud cover only if the temperature reading in band 4 should be
      greater than 245 K. 
      
       
      ·        
      High Reflective Background test: It also usual for bare soil (i.e., sandy beach) to
      give high band 3 temperature readings. We only can differentiate between
      fire and bare soil by the visible band 1. Band 1 gets high visible
      reflectance from bare soils, unlike forest fires, which give much lower
      visible reading. Thus, when band 1 is less than 0.25, it means the pixel
      is not bare soil.   
      
       
      ·        
      Glitter test: Sometimes, water surfaces under sun glint can have similar spectral
      response patter to this of forest fire. But, fires give different readings
      for band 1 and band 2, more than 0.01. So, to exclude water surfaces under
      glint condition, we subtract the reflectance of band 1 and band 2. If the
      difference is more than 0.01, the pixel is not water surface.  
      
       
      ·       
      Visual inspection: The tests above don’t include every fire and exclude every other
      unrelated earth object. Unrealistic detection is till present, while some
      highly probable fires are still lost. The visual inspection is needed to
      cancel dubious cases (e.g., large uniform zone taken as fire). In the
      examining of 4000 images, the visual inspection led to the rejection of
      10% of the images, because environmental problems were marked as fire.       
        
      Limitations 
      
      
      In addition to the environmental problems, there are
      some types of problems and limitations. Some of them are as follows:
      
       
      1        
      Cloud
      cover can be so huge that it covers a significant part of the study area.
      This becomes troublesome, because all the area covered is completely
      discarded from the study as non-accessible.
      
       
      2        
      The
      fire temperature relative to its extent might be insufficient to mark the
      pixel as fire.
      
       
      3        
      The
      orbit of the satellites may drift, which produces different reading from
      one year to another.
      
       
      4        
      The
      images are corrected from distortion caused by atmospheric objects, e.g.,
      aerosols.  
       
       
       
      
        
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