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7th Workshop on Forest Fire Management - EARSeL, European ...

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60<br />

I - PRE-FIRE PLANNING AND MANAGEMENT<br />

Raster layer 1<br />

Raster layer 2<br />

Pixel c<strong>on</strong>taining the value 2236634<br />

Where 2 = geoclimate unit (central alpine)<br />

2 = deep m<strong>on</strong>tane (900 – 1100 m)<br />

3 = crown closure (moderate)<br />

6 = vegetati<strong>on</strong> type (gras)<br />

211= fire ID<br />

Pixel c<strong>on</strong>taining the value 2711634<br />

Where 2 = slope (20 - 30 °)<br />

7 = aspect (west)<br />

1 = deciduous (10%)<br />

1 = c<strong>on</strong>iferous (10%)<br />

634 = fire ID<br />

These two obtained raster layers were then used to highlight patterns of<br />

similar forest and topographic parameters within the fire buffer. To do so,<br />

raster values and their frequencies had to be exported into a database system<br />

where the single parameters could be accessed via SQL language. With<br />

SQL querries it was possible to identify parameters which occurred more<br />

often than others.<br />

One problem arise in this scenario; in very heterogeneous topographic landscapes<br />

the size of a buffer directly influences the amount of pixels and<br />

hence the variance of the value in that buffer. So in very big buffer which<br />

exist when localisati<strong>on</strong> was <strong>on</strong>ly very roughly possible informati<strong>on</strong> get lost<br />

due to no possible identificati<strong>on</strong> of trends. To solve that problem classes of<br />

buffer size were build and individually analyzed. It showed out that with<br />

smaller buffer (< 300m) trends were becoming more visible and for further<br />

analysis <strong>on</strong>ly buffers till 300 meter were c<strong>on</strong>sidered.<br />

Diagram 1 - Vegetati<strong>on</strong><br />

compositi<strong>on</strong> in burned<br />

areas.

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