indices and transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · the...

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Indices and Transforms Ratios … enhance albedo contrasts by reducing inter-band similarities e.g. Near-IR / Red to identify vegetation e.g. Red / Mid-IR to identify snow / ice Ratio Vegetation Index (RVI) = Near IR / Red …… < 1 = unvegetated * RVI can create infinite values Difference Vegetation Index (DVI) = NIR - Red …… < 0 = unvegetated * DVI is influenced by different lighting

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Page 1: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Indices and Transforms

Ratios… enhance albedo contrasts by reducing inter-band similarities

e.g. Near-IR / Red … to identify vegetation

e.g. Red / Mid-IR … to identify snow / ice

Ratio Vegetation Index (RVI) = Near IR / Red …… < 1 = unvegetated

* RVI can create infinite values

Difference Vegetation Index (DVI) = NIR - Red …… < 0 = unvegetated

* DVI is influenced by different lighting

Page 2: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Normalised Difference Vegetation Index: NDVI

Page 3: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Normalised Difference Vegetation Index NDVI

Division compensates for differential Illumination and yields values between-1 and 1, … in a 32 bit channel

It gives a close estimate of biomassalso referred to as greenness

Negative values of NDVI (values approaching -1) correspond to water.

Values close to zero (-0.1 to 0.1) = barren areas of rock, sand, or snow.

low, positive values represent shrub and grassland (~ 0.2 to 0.5),

high values indicate temperate and tropical rainforests (0.6 to 0.9)

Page 4: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

The difference between the

average NDVI for a particular

month of a given year (such

as August 1993, above) and

the average NDVI for the

same month over the last 20

years is the NDVI anomaly. In

1993, heavy rain in the

Northern Great Plains led to

flooding in the Missouri River.

The resulting exceptionally

lush vegetation appears as a

positive anomaly (green).

Annual and interannual chnages in NDVI

Page 5: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

http://phenology.cr.usgs.gov/ndvi_foundation.php

Many satellite sensors have red and Near IR bands to assess global vegetation

Page 6: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Special sensors for NDVI

SPOT 5 has extra bands / wide sensor in visible/NIR with 1 km resolution to capture a repeat 2400 km swath for global coverage

MODIS and NOAA-AVHRR have 250m/1000m red /near-IR bands for NDVI

NDVI is used to measure vegetation amount or biomass, in regional and global estimates. "NDVI is directly related to photosynthesis and thus energy absorption of plant canopies"

Global NDVI change: https://archive.org/details/SVS-3584

Page 7: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Delineation of Grizzly Bear Habitat in Bute InletGEOG432 project

Sieved maximum NDVI result

Page 8: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

http://www.grayhawk-imaging.com/useofndviimagery.html

Page 9: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

The use of NDVI to determine vegetative green-up after a forest fire Geog432

1987 2002

NDVI NDVI

Page 10: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

The use of NDVI to determine vegetative green-up after a forest fire

NDVI difference – 1987-2002

Red - Negative Growth Range Clear - Neutral Growth Range

Yellow - Minimal Positive Growth Orange - Maximum Positive Growth

Page 11: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

http://abstracts.rangelandmethods.org/doku.php/remote_sensing_methods:normalized_burn_ratio

Similar indices: Normalised Burn Ratio (Index)(Near IR – Mid-IR) / (Near IR + Mid-IR) Landsat TM: NBR = (4-7)/(4+ 7)

Page 12: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Other indices include:

Soil-adjusted Vegetation Index (SAVI) = 1.5 * (NIR - R) / (NIR + R + 0.5)

Optimised Soil-adjusted Vegetation Index (OSAVI) = (NIR - R) / (NIR + R + 0.16)

-----------------------------------------------------------------------------

Green: NDGI= (NIR-G) / (NIR+G) TM = (4-2)/ (4+2)

Snow: NDSI = (Green-MIR) / (Green+MIR) TM = (2-5) / (2+5)

Water: NDWI = (NIR – MIR)/ (NIR + MIR) TM = (4-5) / (4+5)

Page 13: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

The technique was named after the pattern of spectral change of agricultural crops during senescence, plotting brightness (visible) against greenness (NIR). The sequence is:

1. Bare fields / newly planted crops - high brightness, low greenness (spring)

2. Plant Growth - <-<- brightness (early summer)

3. Maturity: -> -> greenness (late summer)

4. Senescence (harvest) - bare field/stubble: <-<-greenness, ->-> brightness (Fall)

Tasseled Cap transformation

Page 14: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Tasseled Cap transformation ArcMap 10.3

|

The Tasseled Cap (Kauth-Thomas) transformation is designed to analyze and

map vegetation and urban development changes detected by satellite sensors.

It is known as the Tasseled Cap transformation due to the data shape.

It was developed in 1976 by R.J. Kauth and G.S. Thomas of the Environmental

Research Institute of Michigan (ERIM). The researchers found the patterns in

Landsat MSS data of agricultural fields as a function of the life cycle of the crop.

Essentially, as crops grow from seed to maturity, there is a net increase in near-

infrared and decrease in red reflectance based on soil color

4:Green 5:Red 6:NIR1 7:NIR2

Page 15: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Tasseled Cap Transformation

MSS data, the 4-band dataset creates channels:

Brightness, Greenness, Yellowness (non-such)

TM data, 6-band (no thermal)

Brightness

Greenness

Wetness (SWIR)

Page 16: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Coastal

Band 1

Blue

Band 2

Green

Band 3

Red

Band 4

NIR

Band 5

SWIR1

Band 6

SWIR2

Band 7

Brightness 0 0.3029 0.2786 0.4733 0.5599 0.5080 0.1872

Greenness 0 -0.2941 -0.2430 -0.5424 0.7276 0.0713 -0.1608

Wetness 0 0.1511 0.1973 0.3283 0.3407 -0.7117 -0.4559

Landsat 8 OLI coefficients

Why are they different at all ?

Page 17: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Tasseled Cap Transformation

Kauth, R. J. and Thomas, G. S., 1976, The tasseled cap --a graphic description of the spectral-temporal development of agricultural crops as seen in Landsat, in Proceedings on the U.S. Department of the Interior 9 U.S. Geological Survey

Symposium on Machine Processing of Remotely Sensed Data, West Lafayette, Indiana, June 29 -- July 1, 1976, 41-51.

Landsat 5 TM coefficients for the Tasseled Cap

Band Brightness Greenness Wetness1 .3037 -.2848 .15092 .2793 -.2435 .19733 .4743 -.5436 .32794 .5585 .7243 .34065 .5082 .0840 -.71127 .1863 -.1800 -.4572

Character: Overall reflectance NIR v Visible MIR v NVIR

Page 18: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Brightness – measure of soil reflectance

Greenness – vegetation

Wetness – soil / canopy moisture

tasseled cap channels 1,2,3

Page 19: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

NDVI v Tasseled Cap greennessboth contrast NIR versus visible reflectance

TCA Greenness is similar to NDVI, with subtle differences and is used in habitat studies.

Figure :John Paczkowski MSc thesis – remote sensing and grizzly bear habitat

Page 20: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

–but only been developed for some sensors…(the coefficients vary according to spectral wavelengths and radiometric resolution)

PCI Geomatica

Landsat 1-3 MSS

Landsat 5 TM

Landsat 7 ETM+

-NOT Landsat 8 OLI / Sentinel 2

Other ?:CBERS-02B (China/Brazil)

Ikonos, Quickbird 2

ASTER / MODIS

Russian tassel cap

Page 21: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Reasons to use Tassel Cap Analysis

It reduces a multi band dataset (4-6) to 3 channels –Brightness, Greenness, Wetness – each might be useful

The 3 channels could be used in classification

The coefficients are universal for each sensor

I can show cute tassel photos

-known as the Tasseled Toque

in Canada (fake RS humour]

http://www.sjsu.edu/faculty/watkins/tassel.htm

Page 22: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

http://eoedu.belspo.be/en/guide/compprin.asp

PCA is a mathematical transformation that converts original data into new data channels that are uncorrelated and minimise data redundancy. Like TCA, it can also: reduce shadows and spectral correlation between bands

Principal Components Analysis (PCA)

Page 23: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

http://geology.wlu.edu/harbor/geol260/lecture_notes/Notes_rs_PC.html

The bands can be reduced to their respective 'components', by an 'axial rotation'

The main axis through the points is a 'component'; if all points were on it, correlation=1, the first component (PC1) would 'explain' all the variation.

The 2nd component (PC2) is normal to PC1, uncorrelated and hence two bands are converted to two components, but most variation is explained by the first (the 2nd is always smaller)

Page 24: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Principal Components Analysis (PCA)

The new channels are defined by eigenvectors / eigenvalues.

In the ‘matrix’:

Eigenvectors: define the contribution of each band

Eigenvalues: ‘explain’ the % variance of each PCA channel

PC1 and PC2 explain 95-99% and PC3 most of the rest

PC1= what is explained in both bands (images)

PC2= what is different between them (similar to a band ratio)

Page 25: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

PCA channels

Eigenvectors of covariance matrix (arranged by rows):TM1 2 3 4 5 6 7

PC1 0.22 0.15 0.29 0.16 0.75 0.33 0.40PC2 -0.28 -0.14 -0.29 0.82 0.23 -0.25 -0.16PC3 0.51 0.31 0.43 0.49 -0.46 -0.05 -0.00PC4 -0.09 -0.09 -0.19 0.19 -0.23 0.91 -0.18PC5 0.31 0.13 0.05 -0.12 0.35 -0.00 -0.86PC6 0.69 -0.16 -0.68 -0.01 0.01 -0.04 0.19PC7 -0.19 0.90 -0.39 -0.04 0.00 0.00 0.06

Component71% Brightness21% Greenness3.8% Swirness / Wetness2.3% Impact of TM61.6% Band 5 v 7 (MIR)0.2% Band 1 v 3 (B v R)0.1% Band 2 v 3 (Yellowness)

PC1: Brightness, PC2: Greenness, PC3: Swirness / Wetness

Page 26: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

PC components PC4: TM6, PC5: TM5/7, PC6: TM1/3, PC7: TM2/3

Page 27: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Differences with Tasseled Cap (TCA) :

1. PCA transformation is scene specific -TCA coefficients are 'global‘

2. PCA generates as many components as there are input channels

- TCA creates three new transformed channels

e.g. for Landsat TM, there could be 7 new component channels

There is a high correlation between all ‘greenness’ channels:-As they all contrast near-IR and visible bands

NDVI 4/3 ratio TCA greenness PCA component 2 (usually)

Page 28: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Decorrelation Stretch: Remote sensing technique to enhance images

- Based on Principal Components Analysis (PCA)

- used to Enhance Rock Art Images By Jon Harman, Ph.D.

Page 29: Indices and Transforms - gis.unbc.cagis.unbc.ca/wp-content/uploads/2013/05/indices2018.pdf · The difference between the average NDVI for a particular month of a given year (such

Face Recognition Using Principal Component Analysis

1: Human-ness (or lack of)

2: Gender (or skin colour)

3: Hair (colour / volume / lack of)

4: Facial hair

5: Mouth – Smile – Teeth - smirk

6-7: Age, Ears, Eyes, Nose … ?