icc 2009, santiago de chile visualization of glacier surface movement samuel wiesmann institute of...

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ICC 2009, Santiago de Chile Visualization of Glacier Surface Movement Samuel Wiesmann Institute of Cartography, ETH Zurich

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ICC 2009, Santiago de Chile

Visualization of Glacier Surface MovementSamuel WiesmannInstitute of Cartography, ETH Zurich

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Outline

Introduction Existing visualizations Describing the data in geographic data cube Shortcomings and problems Approach Outlook Conclusions

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Introduction

Visualization of glacier surface movement:

Ice flow: velocities

Changes in ice thickness

Changes in glacier length andice covered area

Mass displacement

(change in shape of crevasses, movement of crevasses, …)

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Existing Visualizations

Vector field … along with isotaches

[Kääb 2005]

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Existing Visualizations

Streamlines and trajectories

[Kääb 2005][NASA SVS 2006/2009]

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Existing Visualizations

Velocities: classified and stretched color ramp

[Quincey et al. 2009]

[Giles et al. 2009]

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Existing Visualizations

Color coded velocities with overlain vectors

[Bolch et al. 2008]

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Existing Visualizations

Velocity vectors and color coded changes in elevation

[Kääb 1997/2005]

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Existing Visualizations

Dynamic arrows depict flow conditions

[NASA SVS 2004/2009]

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Existing Visualizations

Movie of 2.5D retreat simulation

[Jouvet 2008]

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Geographic Data Cube

The principle I

Time

Variable

Space

point in time (t1)

specific area, e.g. glacier surface

variables from glacier surface (velocity, height, temperature, …)

adopted from [Bahrenberg et al. 1990], [Maidment et al. 2002]

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The principle II

Geographic Data Cube

e.g. velocity

point in time (t1)

Time

Variable

Space

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Situation in a glacier map

Geographic Data Cube

Time

Variable

Space

velocity

heights a.s.l.

direction

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Geographic Data Cube

Type 1: ca. 50% of analyzed visualizations (N=80) fixed space, 1 point in time, 1 to 4 variables

Time

Variable

Space

[Kääb 2005]

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The second type I

Geographic Data Cube

Time

Variable

Space

velocity

heights a.s.l.

direction

point in time (t1)

point in time (t2)

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The second type II

Geographic Data Cube

Time

Variable

Space

velocity

heights a.s.l.

direction

point in time (t1)

point in time (t2)

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Geographic Data Cube

Type 2: ca. 40% of analyzed visualizations (N=80) fixed space, 2 (or more) points in time,

1 to 3 variables (whereof 1 at different times)

[NASA SVS 2006/2009]

Time

Variable

Space

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Geographic Data Cube

Type 1: ca. 50% (N=80)

Type 2: ca. 40%

Type 3: ca. 10%fixed space, time animated, usually 1 variable

Time

Variable

Space

Time

Variable

Space

Time

Variable

Space

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Situation summarized

0% allowing for spatial navigation

0% allowing for thematic navigation

10% allowing for temporal navigation (usually start/stop)

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Problems which arise

Overlaying symbols when comparing: 1 position (X/Y), 3 values

[Kääb 1996]

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Problems which arise

Overlaying symbols when comparing: e.g. feature tracking: 4 positions (X/Y), 4 values

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Main problems

Problem of scale

Integration of time

[Pritchard et al. 2005]

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Approach

Intended system architecture

DBMS

PostgreSQLand PostGIS

Preprocessing

Userweb-browser

GIS-Server

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Outlook I

Testing different visualization techniques How to improve? 2D or 3D -- 2D and 3D?

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Outlook II

A lot of data from many projects Usually processed for only one publication

Bundle the data and re-use it!

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Outlook III

Compare two glaciers at a certain date Monitor a glacier over a specific time period Compare two glaciers over this period of time

Calculate differences Interpolation

Profiles on-the-fly

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Outlook IV

Integration of glacier simulation models

Extract potentially dangerous areas

Resource when estimating potential natural hazards

… and many more …

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Conclusions

Glaciology mostly uses “classic” cartography Bundle the data! GIS and cartography may provide the platform Underlying technique exists and is ready to adapt Improving the visualization and combining tools More efficient gain of knowledge in glaciology

ICC 2009, Santiago de Chile

Visualization of Glacier Surface MovementSamuel [email protected]

Thank you for your attention

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Existing Visualizations

Partially dynamic and interactive visualization

[Isakowski 2003]

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Data Cube - Time

1 specific point in time anywhere in space any variable Time

Variable

Space

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Data Cube - Space

1 specific location X/Y/Z any point in time any variable Time

Variable

Space

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Data Cube - Variable

1 specific variable any point in time anywhere in space Time

Variable

Space