cleargif

 

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cleargif

 

cleargif

cleargif

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.