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Advanced Landslide Assessment of the
                       Halenkovice Experimental Site
                                          Miloš Marjanović




This presentation is co-financed by the
European Social Fund and the state
budget of the Czech Republic
Introduction
   Motifs:
       raising awareness
       need for diverse case studies at different
        scales, using different methods
       applicability (decision making for land use planning and civil protection)

   Objectives:
       reliability and coherency of inputs (specially landslide inventory)
       performing advanced modeling (many different methods)
       evaluating models in the best fashion
       providing maps/models as final outputs to be used in
        practical/scientific manner



                     First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Introduction
   Landslides – mass movements of the ground

   Landslide susceptibility – spatial probability
    of landslide occurrence (relation to hazard, risk…)

   Setting definition:
       Classification after Varnes 1978 (defining the mechanism and typology)
       Scale/resolution (mid-scale, after Fell et all 2008)
       Raster format data structure, pixel resolution 10 m
       Definition of geometry (size, depth, area, frequency of landslides)


                    First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Introduction
   Problems & perspectives in landslide assessment

       lack of data, lack of possibility to relate events with triggers, non-
        linearity of the problem…

       piling investigations, promising capacities for monitoring (ground
        sensors and Remote Sensing) in the future




                     First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Methodology
   Methods for data pre-processing and selection:                 q     n      (ϕ oi , j − ϕ ei , j )2
                                                        Χ =∑             ∑
         Chi-square
                                                          2
                                                                  i=1   j =1          ϕ ei , j

         Entropy
                                                                                     k   ni      n
                                                         E ( Sin ) = −∑
                                                                                         N
                                                                                            log 2 i
                                                                                                 N
                                                                                    i =1


   Landslide modeling methods                                                                                 ADVANCED!
        Deterministic, Heuristic, Statistical, Fuzzy, Machine Learning
   Methods for data evaluation
        ROC plot
        Kappa-index

                n              n                    n
        κ =(   ∑
               i =1
                      xii −   ∑
                              i =1
                                     yii ) /(1 −   ∑y )
                                                   i =1
                                                              ii




                                               First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Methodology
 Machine learning - Support Vector Machines
 (SVM)
    Classification task
    Optimization (only two parameters)
    Training over sampling splits
    Testing the rest of the dataset with trained classifier
    Kernels




               First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Methodology
                     support vectors



              landslide
e.g. aspect




                                                            e.g. aspect
                                                    stable




                   e.g. slope                                                    e.g. slope


                          First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Methodology
   Experiment design


      SAGA




                                                                            SAGA


              First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Methodology
   Experiment design
       Testing
       Cross-Validation
       Training




                  First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset
   Study Area




                 First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset
   Landslide Inventory
       CGS survey (1:10 000)
        http://mapy.geology.cz/svahove_nestability/

       Field investigation
           Independent field survey
           Continuation from previous studies at the department
            (Křivka, Marek, Bíl)




                     First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset




          First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset




          First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset




          First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset




          First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset




          First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset
   Thematic attributes                           #    attribute                               source

       Morphometric attributes                   1    DEM                                     Topo-maps
                                                  2    Slope                                   DEM
       Hydrological attributes                   3    Slope length                            DEM
       Environmental attributes                  4    Aspect                                  DEM

       Geological attributes                     5    Plan/profile curvature                  DEM
                                                  6    Convergence index                       DEM
                                                  7    Drainage elevations                     DEM
                                                  8    Elevation above drainage                DEM
                                                  9    Drainage buffer                         DEM

                                                  10   LS factor                               DEM

                                                  11   TWI                                     DEM

                                                  12   Catchment area                          DEM

                                                  13   Land cover units                        Orthophoto
                          nominal
                                                  14   Lithological units                      Geo-maps


                  First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Dataset
   Attribute layers




                First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Results
   Model accuracy
=== Summary ===

Correctly Classified Instances 304080 = 88.16 %
Incorrectly Classified Instances 40814 = 11.83 %
Kappa statistic                   0.1025
Mean absolute error               0.1183
Root mean squared error           0.344
Relative absolute error           75.3045 %
Root relative squared error       136.5789 %
Coverage of cases (0.95 level) 88.1662 %
Mean rel. region size (0.95 level) 50 %
Total Number of Instances          344894

=== Detailed Accuracy By Class ===

 TP Rate FP Rate   Precision Recall F-Measure MCC ROC Area PRC Area Class
    0.932 0.823    0.941    0.932 0.936   0.103 0.555 0.94  0
    0.177 0.068    0.156    0.177 0.166   0.103 0.555 0.082 1
Avg.0.882 0.773    0.889    0.882 0.885   0.103 0.555 0.883

=== Confusion Matrix ===

   a     b <-- classified as: a=non-landslide
300020 21980 |   a=0          b=landslide
 18834 4060 |    b=1




                              First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Case Study Results
   Comparison with an earlier, non-predictive model based
    on multivariate regression




               First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Conclusions
   Overall:
       model seems promising, but there is room for improvements
       the study is in its beginning and it might be interesting to extend
        it methodologically and to compare the results
   Drawbacks
       bad communication between GIS and Machine Learning platform
       time consumption
   For further notice:
       it is necessary to increase the number of folds in optimization
       it would be interesting to challenge the algorithm with multi-
        class (multinomial) scenario
       post-procesing might be good refinement for the overall
        accuracy First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
Advanced Landslide Assessment of the
Thank You For Your Attention!
          Halenkovice Experimental Site
                                                     Miloš Marjanović
                                          milos.marjanovic01@upol.cz




This presentation is co-financed by the
European Social Fund and the state
budget of the Czech Republic

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Marjanović, M: Advanced Landslide Assessment of the Halenkovice Experimental Site

  • 1. Advanced Landslide Assessment of the Halenkovice Experimental Site Miloš Marjanović This presentation is co-financed by the European Social Fund and the state budget of the Czech Republic
  • 2. Introduction  Motifs:  raising awareness  need for diverse case studies at different scales, using different methods  applicability (decision making for land use planning and civil protection)  Objectives:  reliability and coherency of inputs (specially landslide inventory)  performing advanced modeling (many different methods)  evaluating models in the best fashion  providing maps/models as final outputs to be used in practical/scientific manner First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 3. Introduction  Landslides – mass movements of the ground  Landslide susceptibility – spatial probability of landslide occurrence (relation to hazard, risk…)  Setting definition:  Classification after Varnes 1978 (defining the mechanism and typology)  Scale/resolution (mid-scale, after Fell et all 2008)  Raster format data structure, pixel resolution 10 m  Definition of geometry (size, depth, area, frequency of landslides) First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 4. Introduction  Problems & perspectives in landslide assessment  lack of data, lack of possibility to relate events with triggers, non- linearity of the problem…  piling investigations, promising capacities for monitoring (ground sensors and Remote Sensing) in the future First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 5. Methodology  Methods for data pre-processing and selection: q n (ϕ oi , j − ϕ ei , j )2 Χ =∑ ∑ Chi-square 2  i=1 j =1 ϕ ei , j Entropy k ni n  E ( Sin ) = −∑ N log 2 i N i =1  Landslide modeling methods ADVANCED!  Deterministic, Heuristic, Statistical, Fuzzy, Machine Learning  Methods for data evaluation  ROC plot  Kappa-index n n n κ =( ∑ i =1 xii − ∑ i =1 yii ) /(1 − ∑y ) i =1 ii First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 6. Methodology  Machine learning - Support Vector Machines (SVM)  Classification task  Optimization (only two parameters)  Training over sampling splits  Testing the rest of the dataset with trained classifier  Kernels First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 7. Methodology support vectors landslide e.g. aspect e.g. aspect stable e.g. slope e.g. slope First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 8. Methodology  Experiment design SAGA SAGA First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 9. Methodology  Experiment design  Testing  Cross-Validation  Training First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 10. Case Study Dataset  Study Area First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 11. Case Study Dataset  Landslide Inventory  CGS survey (1:10 000) http://mapy.geology.cz/svahove_nestability/  Field investigation  Independent field survey  Continuation from previous studies at the department (Křivka, Marek, Bíl) First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 12. Case Study Dataset First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 13. Case Study Dataset First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 14. Case Study Dataset First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 15. Case Study Dataset First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 16. Case Study Dataset First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 17. Case Study Dataset  Thematic attributes # attribute source  Morphometric attributes 1 DEM Topo-maps 2 Slope DEM  Hydrological attributes 3 Slope length DEM  Environmental attributes 4 Aspect DEM  Geological attributes 5 Plan/profile curvature DEM 6 Convergence index DEM 7 Drainage elevations DEM 8 Elevation above drainage DEM 9 Drainage buffer DEM 10 LS factor DEM 11 TWI DEM 12 Catchment area DEM 13 Land cover units Orthophoto nominal 14 Lithological units Geo-maps First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 18. Case Study Dataset  Attribute layers First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 19. Case Study Results  Model accuracy === Summary === Correctly Classified Instances 304080 = 88.16 % Incorrectly Classified Instances 40814 = 11.83 % Kappa statistic 0.1025 Mean absolute error 0.1183 Root mean squared error 0.344 Relative absolute error 75.3045 % Root relative squared error 136.5789 % Coverage of cases (0.95 level) 88.1662 % Mean rel. region size (0.95 level) 50 % Total Number of Instances 344894 === Detailed Accuracy By Class === TP Rate FP Rate Precision Recall F-Measure MCC ROC Area PRC Area Class 0.932 0.823 0.941 0.932 0.936 0.103 0.555 0.94 0 0.177 0.068 0.156 0.177 0.166 0.103 0.555 0.082 1 Avg.0.882 0.773 0.889 0.882 0.885 0.103 0.555 0.883 === Confusion Matrix === a b <-- classified as: a=non-landslide 300020 21980 | a=0 b=landslide 18834 4060 | b=1 First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 20. Case Study Results  Comparison with an earlier, non-predictive model based on multivariate regression First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 21. Conclusions  Overall:  model seems promising, but there is room for improvements  the study is in its beginning and it might be interesting to extend it methodologically and to compare the results  Drawbacks  bad communication between GIS and Machine Learning platform  time consumption  For further notice:  it is necessary to increase the number of folds in optimization  it would be interesting to challenge the algorithm with multi- class (multinomial) scenario  post-procesing might be good refinement for the overall accuracy First InDOG Doctoral Conference, 29th October - 1st November 2012, Olomouc
  • 22. Advanced Landslide Assessment of the Thank You For Your Attention! Halenkovice Experimental Site Miloš Marjanović milos.marjanovic01@upol.cz This presentation is co-financed by the European Social Fund and the state budget of the Czech Republic