geog2021 environmental remote sensing lecture 3 spectral information in remote sensing

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GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

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Page 1: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

GEOG2021Environmental Remote Sensing

Lecture 3

Spectral Information in Remote Sensing

Page 2: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Aim

• Mechanisms variations in reflectance - optical/microwave

• Visualisation/analysis

• Enhancements/transforms

Page 3: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Mechanisms

Page 4: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Reflectance

• Reflectance = output / input• (radiance)• measurement of land complicated by atmosphere

• input solar radiation for passive optical

• input from spacecraft for active systems• RADAR

– Strictly NOT reflectance - use related term backscatter

Page 5: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Mechanisms

Page 6: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Optical Mechanisms

Page 7: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Reflectance

causes of spectral variation in reflectance

• (bio)chemical & structural properties – chlorophyll concentration – soil - minerals/ water/ organic matter

Page 8: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Optical Mechanisms

vegetation

Page 9: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Optical Mechanisms

soil

Page 10: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Optical Mechanisms

soil

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RADAR Mechanisms

See: http://southport.jpl.nasa.gov/education.html

Page 12: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

RADAR Mechanisms

Page 13: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

RADAR Mechanisms

Page 14: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

RADAR Mechanisms

Page 15: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Vegetation amountconsider

• change in canopy cover over time

• varying proportions of soil / vegetation (canopy cover)

Page 16: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Vegetation amount

Bare soil

Full cover

Senescence

Page 17: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Vegetation amount

1975 Rondonia See: e.g. http://earth.jsc.nasa.gov/lores.cgi?PHOTO=STS046-078-026

http://www.yale.edu/ceo/DataArchive/brazil.html

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Vegetation amount

1986 Rondonia

Page 19: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Vegetation amount

1992 Rondonia

Page 20: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Uses of (spectral) information

consider properties as continuous – e.g. mapping leaf area index or canopy cover

or discrete variable – e.g. spectrum representative of cover type

(classification)

Page 21: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing
Page 22: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Leaf Area Index

See: http://edcdaac.usgs.gov/modis/dataprod.html

Page 23: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Forest cover 1973

See: http://www.bsrsi.msu.edu/rfrc/stats/seasia7385.html

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Forest cover 1985

Page 25: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysis• spectral curves

– spectral features, e.g., 'red edge’

• scatter plot– two (/three) channels of information

• colour composites – three channels of information

• principal components analysis

• enhancements – e.g. NDVI

Page 26: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysis• spectral curves

– reflectance (absorptance) features – information on type and concentration of

absorbing materials (minerals, pigments) • e.g., 'red edge':

increase Chlorophyll concentration leads to increase in spectral location of 'feature'

e.g., tracking of red edge through model fitting or differentiation

Page 27: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysis

Page 28: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysis

Page 29: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing
Page 30: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

http://envdiag.ceh.ac.uk/iufro_poster2.shtm

Page 31: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

REP moves to shorter

wavelengths as chlorophyll decreases

Red Edge Position

point of inflexion on red edge

Page 32: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

REP correlates with ‘stress’,

but no information on

type/cause

Measure REP e.g. by 1st

order derivative

See also: Dawson, T. P. and Curran, P. J., "A new technique for interpolating the reflectance of red edge position." Int. J. Remote Sensing, 19, (1998),2133-2139.

Page 33: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Consider red / NIR ‘feature space’

Soil line

vegetation

Page 34: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysis• Colour Composites

• choose three channels of information– not limited to RGB– use standard composites (e.g., FCC)

• learn interpretation

Page 35: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisStd FCC - Rondonia

Page 36: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisStd FCC - Swanley TM data - TM 4,3,2

Page 37: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– PCA (PCT - transform)

• may have many channels of information– wish to display (distinguish)– wish to summarise information

• Typically large amount of (statistical) redundancy in data

Page 38: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

red NIR

See: http://rst.gsfc.nasa.gov/AppC/C1.html

Page 39: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

red

NIR

Scatter Plot reveals relationship between information in two bands

here:

correlation coefficient = 0.137

Page 40: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– show correlation between all bands

TM data, Swanley:

correlation coefficients : 1.000 0.927 0.874 0.069 0.593 0.426 0.736 0.927 1.000 0.954 0.172 0.691 0.446 0.800 0.874 0.954 1.000 0.137 0.740 0.433 0.812 0.069 0.172 0.137 1.000 0.369 -0.084 0.119 0.593 0.691 0.740 0.369 1.000 0.534 0.891 0.426 0.446 0.433 -0.084 0.534 1.000 0.671 0.736 0.800 0.812 0.119 0.891 0.671 1.000

Page 41: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– particularly strong between visible bands– indicates (statistical) redundancy

TM data, Swanley:

correlation coefficients : 1.000 0.927 0.874 0.069 0.593 0.426 0.736 0.927 1.000 0.954 0.172 0.691 0.446 0.800 0.874 0.954 1.000 0.137 0.740 0.433 0.812 0.069 0.172 0.137 1.000 0.369 -0.084 0.119 0.593 0.691 0.740 0.369 1.000 0.534 0.891 0.426 0.446 0.433 -0.084 0.534 1.000 0.671 0.736 0.800 0.812 0.119 0.891 0.671 1.000

Page 42: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– PCT is a linear transformation– Essentially rotates axes along orthogonal axes

of decreasing variance

red

NIR

PC1

PC2

Page 43: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– explore dimensionality of data

% pc variance :

– PC1 PC2 PC3 PC4 PC5 PC6 PC7

– 79.0 11.9 5.2 2.3 1.0 0.5 0.1

96.1%

of the total data variance contained within the first 3 PCs

Page 44: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– e.g. cut-off at 2% variance– Swanley TM data 4-dimensional

• first 4 PCs = 98.4%

– great deal of redundancy TM bands 1, 2 & 3

correlation coefficients : 1.000 0.927 0.874 0.927 1.000 0.954

0.874 0.954 1.000

Page 45: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– display PC 1,2,3 - 96.1% of all data variance

Dull -

histogram equalise ...

Page 46: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– PC1 (79% of variance)

Essentially

‘average brightness’

Page 47: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

stretched sorted eigenvectors

PC1 +0.14 +0.13 +0.28 +0.13 +0.82 +0.12 +0.43

PC2 -0.44 -0.27 -0.60 +2.23 +0.47 -0.49 -0.77

PC3 +1.68 +1.35 +2.45 +1.34 -1.49 -0.67 +0.05

PC4 +0.29 +0.10 -1.22 +1.90 -1.83 +4.49 +2.30

PC5 +0.03 -0.39 -2.81 +0.70 -1.78 -5.12 +6.52

PC6 10.42 +1.10 -6.35 -0.70 +1.64 -0.23 -2.39

PC7 -8.77 28.50 -8.37 -1.43 +1.04 -0.40 -1.75

Page 48: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

• shows contribution of each band to the different PCs. – For example, PC1 (the top line) almost equal

(positive) contributions (‘mean’)PC1 +0.14 +0.13 +0.28 +0.13 +0.82 +0.12 +0.43

– PC 2 principally, the difference between band 4 and rest of the bands (NIR minus rest)

PC2 -0.44 -0.27 -0.60 +2.23 +0.47 -0.49 -0.77

Page 49: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

visualisation/analysisPrincipal Components Analysis

– Display of PC 2,3,4

Here, shows

‘spectral differences’

(rather than ‘brightness’

differences in PC1)

Page 50: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

– reexamine red/nir space features

Page 51: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

– define function of the two channels to enhance response to vegetation & minimise response to extraneous factors (soil)

– maintain (linear?) relationship with desrired quantity (e.g., canopy coverage, LAI)

Page 52: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

– function known as ‘vegetation index’– Main categories:

• ratio indices (angular measure)

• perpendicular indices (parallel lines)

Page 53: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

RATIO

INDICES

Page 54: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

– Ratio Vegetation Index • RVI

– Normalised Difference Vegetation Index • NDVI

RATIO

INDICES

Page 55: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

NDVI

RATIO

INDICES

Page 56: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

NDVI

RATIO

INDICES

Page 57: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

RATIO

INDICES

NDVI over Africa (AVHRR-derived) Tucker et al. - A: April; B: July; C: Sept; D: Dec 1982

Page 58: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

PERPENDICULAR

INDICES

Page 59: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

EnhancementsVegetation Indices

– Perpendicular Vegetation Index • PVI

– Soil Adjusted Vegetation Index• SAVI

PERPENDICULAR

INDICES

Page 60: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

PERPENDICULAR

INDICES

And others ...

Page 61: GEOG2021 Environmental Remote Sensing Lecture 3 Spectral Information in Remote Sensing

Summary

• Scattering/reflectance mechanisms

• monitoring vegetation amount

• visualisation/analysis– spectral plots, scatter plots, PCA

• enhancement– VIs