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Using Artificial Intelligence to forecast the location of - - PowerPoint PPT Presentation

Using Artificial Intelligence to forecast the location of earthquake- and post-earthquake-induced landslides r.huso@gns.cri.nz GNS Science Contents Development of an Earthquake-Induced Landslide (EIL) forecast tool for NZ Model


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Using Artificial Intelligence to forecast the location of earthquake- and post-earthquake-induced landslides

r.huso@gns.cri.nz

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Contents

  • Development of an Earthquake-Induced Landslide (EIL) forecast

tool for NZ

  • Model Structure and Training
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AI versus Log Regression

AI model Log Regression model

0.2 0.4 0.6 0.8 1 0.2 0.4 0.6 0.8 1

True positive rate False positive rate

Log Re gres sion - K aikoura trained AI - Murchis

  • n a

nd Ina ng ahua trained

  • AI model trained on Inangahua and Murchison EQ landslide

datasets, then used to forecast Kaikoura EQ landslides

  • Log Regression model trained on Kaikoura EQ and landslides
  • nly
  • AI model statistically preforms well in forecasting Kaikoura EQ

landslides

ROC curve showing model performance

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  • Variables investigated (12)
  • Variables with statistical significance:

– Slope angle – Distance to surface fault rupture – Elevation – Geology – PGA or PGV – LSR: Local Slope Relief

Faults Landslides

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Data Difficulties

  • Data discontinuities and one-hot encoding

– Natural ordinal relationship between the categories?

  • ‘cold’, warm’, and ‘hot’

– Not suitable for one-hot encoding

  • Quaternary gravel, debris, sand
  • Neogene siltstone, sandstone
  • Cretaceous conglomerate, igneous rocks, limestone, mudstone, siltstone
  • Early Cretaceous igneous rocks
  • Paleogene igneous rocks, limestone, limestone
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Data Difficulties (2)

  • Data scales

– Distance (~100,000 m) – Elevation (~2000 m) – LSR (~200) – PGA (~100) – Slope (~90) – GeolCode (1, 2, 3, 4, 5)

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Data discontinuities

GroupInputData Config.json ScaleInputData CaptureDataLimits HyperCubeSmoothing

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Structure Difficulties

  • Model structure

– Number of hidden layers – Number of nodes per layer – Amount of “Dropout”

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Structure Difficulties

HyperparameterOpt Config.json HyperparameterOpt OptimalEpochs

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Model Training and Testing

  • Train the model
  • Apply to Out Of Sample data (if any)
  • Rank the input features
  • Show charts
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Model Training and Testing

Config.json TrainModel TrainModel ApplyModel FeatureRanking ShowCharts

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Model Charts – Confusion Matrix

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Model Charts – Receiver Operating Characteristic

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Model Charts – Receiver Operating Characteristic

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Summary

  • Rapid forecasts of landslide probability and impacts in near-real

time (5-7 minutes) after an event would help to focus such response efforts

  • Several discrete steps are required to produce a useful model that

can be applied when an earthquake event happens

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Questions

r.huso@gns.cri.nz