17
Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Embed Size (px)

DESCRIPTION

Volcán de Colima Compare simulation with real event of a block and ash flow –April of 1991

Citation preview

Page 1: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Procedure to Compare Numerical Simulation of Geophysical Flow

with Field Data

Laércio M. NamikawaGeo559 - Spring2004

Page 2: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Objective

• Develop a quantitative procedure to compare output of a numerical simulation of geophysical flow with fieldwork data.

• Geophysical flow challenges for comparison:– Large scale phenomena:

• Knowledge of variables is limited.– Low recurrence

• Small number of real cases.– Dynamic nature:

• Requires analysis of a series of data, each from different time

Page 3: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Volcán de Colima

• Compare simulation with real event of a block and ash flow– April of 1991

http://www.gomanzanillo.com/old_articles/volcano/volfire.htm

Page 4: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Titan2D Simulation• DEM, Internal Friction, Bed Friction• Starting Location, Shape, Volume

Page 5: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Model Performance Measure• Constraints:

– Data from real event is a footprint of flow path;

– Simulation results are available in a series of adapted grids with flow pile height at every time of the simulation.

Page 6: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Proposed Measurement Procedure

• Create a summary of simulation results;

• Define a map with distances to real event flow footprint;

• Apply quantitative analysis using statistics and spatial database approach.

Page 7: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Summary of Simulation ResultsProblems

• Huge amount of data:– 200 files, one for each simulation time step.– 400 Mbytes total.

• Complex structure: Adaptative grid.

Page 8: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Summary of Simulation ResultsSolution

Create GRID with cells equal to zero;For each file: Build irregular mesh; For each mesh element: If rectangular element: For each cell inside element:

Calculate pile height using linear interpolation;Cell value is the highest between calculated and previous.

If triangular element: For each cell inside element:

Calculate pile height using linear interpolation;Cell value is the highest between calculated and previous.

Page 9: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Create Map with Distances to Real Event Flow

• Scan and georeference flow map;

• Digitize flow polygons;• Create skeleton lines

using Delaunay triangulation;

• Create distance to flow center, to flow polygon outline, and composed (center+outline) distance.

Page 10: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Quantitative AnalysisTest Cases

• Best – generated from real flow.

• Second best – “shorter” version of Best.

• Third – simulation.

• Worst – simulation with a very large volume.

Page 11: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Quantitative Analysis Using Statistics and Spatial Database

Approach

• Divide area in analysis units;• For each unit, acquire attributes:

– Mean:• Pile height;• Distance to flow center;• Distance to flow outline;• Composed distance (center+outline).

• Find correlation among attributes;• Select correlation which better fits test

cases.

Page 12: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Analysis UnitsUnit:100 by 100 meters

Page 13: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Find Correlation

Normal Distribution of ResidualsPile height Natural Log

Pile height

Distance Natural LogDistance

Convert distances and pile height to natural log of distances and pile height.

Page 14: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Find Correlation Linear Regression

Assumption: Small pile height at great distances indicates good model performance.

Dependent variable:Pile height

Best predictor:Combined distance center+edge

Problem: Regression line slope increases from Third Best to Worst case.

Diagnosis: Regression is representing only total pile height in the whole area, with no relationship with morphology of the flow.

Page 15: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Logistic Regression

• Assumption: Small pile height outside flow path indicates good model performance.

– Dependent variable: InFlow (1: Inside; 0: Outside)– Predictor: Pile height.

• Problem: Pile height for probability equal to 0.5 Third Best is lower than for Best and Second best cases.

• Diagnosis: Regression is representing only the total pile height in the whole area, with no relationship with morphology of the flow.

• Solution: Include distance in regression.– Regression significance test: Only combined distance is

significant in all cases.

Page 16: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Logistic RegressionDependent variable: InFlow

1: Inside real event flow footprint;0: Otherwise.

Predictors: Pile height;Combined distance: center+outline

Probability of Being Inside Flowat 200 meters from center

0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

PileHeig

ht1.8 3.8 5.8 7.8 9.8 11

.813

.815

.817

.8

Pile Height (m)

Prob

abiit

y p(sim1)

p(sim2)

p(feb22)

p(feb10)

Probability of a Pile 5 Meter High Being Inside Flow

0

0.2

0.4

0.6

0.8

1

Distanc

e 50 100

150

200

250

300

350

400

450

Distance from Flow Center (m)

Prob

abiit

y p(sim1)

p(sim2)

p(feb22)

p(feb10)

sim1 sim2

feb22 feb10

Page 17: Procedure to Compare Numerical Simulation of Geophysical Flow with Field Data Laércio M. Namikawa Geo559 - Spring2004

Conclusion• Quantitative performance measure:

– Logistic Regression with InFlow depending on pile height and combined distance.

• Combination of distances center+outline captures the morphology of flow footprint.

• Performance measures should consider unique characteristics of the phenomena, available data, and model.