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Methods of fire situation analysis

Sakhalin (3K/45K)
Pic. 1. Area of Sakhalin Island covered in fire analysis.

Clic picture for detale map (45 Êá)

Analysis of the fire situation on Sakhalin and the Far East was carried out by R&DC ScanEx, specializing in satellite image processing, at the request of Greenpeace Russia. Satellite images from Resource-01 and NOAA satellites were used in the study. Scanners of Resource-01 satellites are capable of receiving 2-4 channel spectral images with average resolution (150 meters) and a field of vision of 600 km from East to West. They also produce high-resolution images of 35x45 m in visible and infrared (IR) spectrum, having a field of vision of 40 km. AVHRR scanners of NOAA satellites create multispectral images having 1100x1100 m resolution and a field of view of up to 2000 km from East to West.

NOAA series images with standard algorithms were used to identify active burn areas. Since this technique can produce errors, every outbreak of fire was verified by a number of subsequent images. Burned areas were identified using distant infrared spectral zones of NOAA images, and then verified by a series of subsequent images. The following images were used for the fire map of Sakhalin and part of the Far East: NOAA images dated September 4, 11, 23, 25, October 13, 22, 26, 27, 28, November 16, 17, 1998. Fire dynamics in a number of cases were verified and corrected by images of 2 spectral zones, of medium and high resolution of Resource-01 satellites, dated June 27, July 1, 7, 14, 17.

Due to the specific nature of capturing satellite imagery and complicating weather conditions, not to mention the haze which hung over Sakhalin for most of the time, we were able to analyze only part of the area. Picture 1 shows the area of Sakhalin analyzed in this report (approximately 87 % of the island's area).

In developing the map, we decided not to include fires on non-forest areas, (e.g. bogs, wetlands, forestless flood plains, stone slopes with no or little forest cover, previously burned territories lacking subsequent growth, logging sites with no growth, etc.) Neither does the applied technology allow to identify and register the areas, covered by ground fires of low intensity and by minor burning, as well as by "grass" fires, for instance spoil banks of railways and agricultural lands.

It is necessary to point out that early-morning distant infrared spectral zone satellite imagery, does not clearly detect sites which have completely stopped burning and smoldering. Therefore, the total estimate of burning areas is somewhat lower due to underreported extinguished fire sites.

(6K/36K)(9K/24K)
Pic. 2. In 1998, smoke cover from fires extended dozens, if not hundreds of kilometers. These images, taken September 25, 1998, clearly depict smoke plumes north of the Nogliki community.
 
Low precision in identifying small fires is characteristic of NOAA low resolution imagery. For instance, an intense fire source on NOAA images covers an entire pixel (an area of about 1.2 square km), even if the real area of fire is just 0, 25 square km. In distant infrared spectral zone, the burn site covers an entire pixel, as long as the real burnt area makes up 60 - 70 % of the pixel. That is why, when deciphering images and numbering the boundaries of fire sites, we corrected the areas, burnt by fire, to smaller ones.

The specific features of images and deciphering technologies do not always allow one to accurately identify remaining unburned area within major fire sites. This situation concerns most of all a cross-country terrain. However, this overestimation of particular fire sites is fully compensated for by those areas burnt by ground fires and not included into the total forest area of analysis due to the above mentioned reasons.

Thus, the estimates of the areas, burnt by fire in Sakhalin in 1998, appear to be minimal.

The work resulted in a computerized map of Sakhalin in MapInfo 4.5 showing marked fire sites, as well as a burn intensity classification: from the first (crown fires) to the fifth (final stage of smoldering).


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