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SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 1 Prof. Dr. Christiana Schmullius Dr. Leif Eriksson, Dipl.-Geogr. Tanja Riedel Dr. Maurizio Santoro, Dr. Christian Thiel Department for Geoinformatics and Remote Sensing Friedrich-Schiller-University Jena, Germany

Prof. Dr. Christiana Schmullius Dr. Leif Eriksson, Dipl

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SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 1

Prof. Dr. Christiana SchmulliusDr. Leif Eriksson, Dipl.-Geogr. Tanja Riedel

Dr. Maurizio Santoro, Dr. Christian Thiel

Department for Geoinformatics and Remote SensingFriedrich-Schiller-University Jena, Germany

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 2

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ERS coherence image

JERS intensity image

Use model to calculate

class means

Maximum LikelihoodClassifier

Iterated ContextualProbability Classifier

(ICP)

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 3

�������������������� ������ �• Histograms vary from scene to scene.

– How to capture variance? From the scenes themselves.

Simulated Histograms of Stem Volume Classes and Overall Class „Forest“.

Characteristic Values

Wagner et al., RSE, 2003

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 4

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• Ground truth data determine model for ERS coherence and JERS-1 intensity

Coherence Model:γ75 .. CharacteristicCoherence Percentile

( ) 1227575 58.033.0)(

v

ev−

⋅⋅++= γγγ

Test data to determine coherency model.

Wagner et al., RSE, 2003

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 5

��� ����������������������( ) ( ) γγγγγ V

v

ev−

∞∞ ⋅−+= 0

750 γγ γγ ⋅+= ba

( ) γγγγ γγVv

ebav−

⋅−++= 7575 )1()(

( ) 1.1227575 581.0330.0)(

v

ev−

⋅⋅++= γγγ

75γγ ≈∞

v = growing stock volume

γ0 = coherence at v = 0 m3/ha (non-forest)

γ∞ = coherence for asymptotic values of v(corresponding to dense forest)

γ75 = value where the coherence distribution reach 75% of the maximum value (see fig.)

Vγ = characteristic v value where the exponential function has decreased by e-1

Wagner et al., RSE, 2003

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 6

( ) σσσσσ Vv

ev−

∞∞ ⋅−+= 00 )(

34.10775

0 46.2)(v

ev−

⋅−= σσ

Wagner et al., RSE, 2003

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SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 7

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SIBERIA classes Land cover type

Water River, lake, inland water

Smooth areas Agricultural fields, river sand bar

Open areas Bogs, meadows, hayfields, pasture, clear-cut, burnt forest, young regrowth

Forest 20-50 m3/ha

Forest 20-50 m3/ha

Forest 50-80 m3/ha

Forest 50-80 m3/ha

Forest>80 m3/ha

Forest >80 m3/ha

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 8

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Radar Image Mosaic

111 Radar Image Maps

Forest Cover Mosaic

96 Forest Cover Maps

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 9

Pang Yong, Annual Progress Report 2004, CAF

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SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 10

The retrieval process can be divided in four parts: 1. Model selection2. Model training3. Retrieval4. Accuracy assessment

Growing stock volume = stem volume [m3/ha]

Leif Eriksson et al., ForestSAT 2005

Stem volume retrieval – Methodology 1

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 11

Regression model

�: coherence

V: growing stock volume

Regression parameters

A: dynamic range

B: slope

C: offset

( ) CeAV VB +∗= ∗γ

Leif Eriksson et al., ForestSAT 2005

Stem volume retrieval – Methodology 2

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 12

Best results for JERS-1:RMSE = 60 m³/haRelative RMSE = 43 %R² = 0.75

Best results for ERS-1/2:RMSE = 57 m³/haRelative RMSE = 37 %R² = 0.73

Leif Eriksson et al., ForestSAT 2005

Stem volume retrieval – Results

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 13

Regression model

JERS-1 coherence

JERS-1 backscatter

SIBERIA algorithm

JERS-1 coherence

JERS-1 backscatter

SIBERIA algorithm

ERS-1/2 coherence

JERS-1 backscatter

Forest inventory

Leif Eriksson et al., ForestSAT 2005

Interferometric Water Cloud Model

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 14

( )Voveg

Vogr

ofor ee ββ σσσ −− −+= 1

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� �����������

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( ) ( )1

1−−−−− −+= αωββ

σσ

γσσ

γγ hjofor

oveg

vegVV

ofor

ogr

grfor eee

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Interferometric Water Cloud Model

Santoro et al., RSE, 2002

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 15

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�������� ������!��������σ 0���#�σ "� ����β ������(σ ο, �$������ ���

Santoro et al., RSE, 2002

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 16

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Error

Local survey

Santoro et al., RSE, 2002

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 17

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Santoro et al., RSE, 2002

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 18

��Model-based retrieval procedure is robust and consistent�Multi-temporal combination to be preferred�C-band „tandem“ coherence: ideal�L-band backscatter: reliable

�Accuracy comparable to ground-based surveys

��Importance of reference ground-truth and SAR data�C-band „tandem“ coherence: depends on weather conditions�L-band backscatter: few images at ideal conditions

Santoro et al., RSE, 2002

Conclusions – Stem volume retrieval

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 19

Test Questions

1)

2)

3)

4)

SAR Day 2 Lecture 4 Introduction to Modelling C. Schmullius 20