Intelligent Systems for Crisis Management by Sisi Zlatanova Rob Peters Arta Dilo & Hans Scholten

Author:Sisi Zlatanova, Rob Peters, Arta Dilo & Hans Scholten
Language: eng
Format: epub
Publisher: Springer Berlin Heidelberg, Berlin, Heidelberg

Landslides

Height

Slope

Aspect

Curvature

Lithology

Rainfalls

Rock falls

0.451

0.795

0.253

0.534

0.615

0.482

Slides

0.515

0.481

0.110

0.554

0.597

0.392

Debris flows

0.190

0.465

0.066

0.568

0.545

0.183

Earth flows

0.813

0.382

0.274

0.493

0.992

0.606

The matrix method is based on the determination of all possible combinations among the classes of the considered factors, and synthetically can be summarized in the following steps:The total surface of the study area matrix (TSM) is obtained by calculating the area occupied by each of the class combinations of the selected factors.

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