maa-57.2040 kaukokartoituksen yleiskurssi general remote sensing image restoration

Maa-57.2040 Kaukokartoituksen yleiskurssi

General Remote Sensing

Image restoration

Autumn 2007

Markus Törmä

[email protected]

Digital image processing

• Image is manipulated using computer

• Image mathematical operation new image

• Application areas:– Image restoration– Image enhancement

– Image interpretation / classification

Image restoration

• Errors due to imaging process are removed

• Geometric errors– position of image pixel is not correct one when

compared to ground

• Radiometric errors– measured radiation do not correspond radiation

leaving ground

• Aim is to form faultless image of scene

Image enhancement• Image is made better suitable for interpretation• Different objects will be seen better

manipulation of image contrast and colors • Different features (e.g. linear features) will be

seen better e.g. filtering methods • Multispectral images: combination of image

channels to compress and enhance imformation– ratio images– image transformations

• Necessary information is emphasized, unnecessary removed


• Analog signal: – phenomena is described of measured

continuosly according to time or space

• Digital signal: – analog signal is sampled with some interval

• 2-dimensional digital signal

digital image


Image functionf(x,y): • Function

according to spatial coordinates x and y

• Value of function in position (x,y) corresponds to brightness of image in corresponding position


• Digital image consists of individual picture elements, pixels, which form discere lattice in spatial domain (x,y)

• Digital image can also be presented using SIN-waves with different frequencies and amplitudes– called frequence domain (u,v)– Fourier transform is used to determine frequencies

• Manipulation of digital image:– Image domain: pixel values are modified directly at iomage

using some algorithm– Spatial domain: frequencies and amplitudes of SIN-waves

are modified

Sources of errorMovement opf imaging platform• Changes in height or speed • Attitude of satellite

Image provider should correct

Instrument• Scanning or measurement principle• Failures of sensors • Production methods or accuracy of instrument

Calibration of instrument

Sources of errorAtmosphere• Attenuation of radiation and decrease of contrast • Image is blurred

Difficult to correct

Object• Roundness of Earth • Rotation of Earth • Topography

It is possible to cerrect these quite well

Geometric correction

• Position of image pixel is not correct when compared to ground

• Errors due to instrument, movement of imaging platform and object are removed

• Known errors in geometry:– Earth cirvature and rotation

– Topography

– Imaging geometry

• Rectification to map projection– Geometric transformation

– Interpolation of pixel digital numbers


• Geometric correction is made – automatically using orbital parameters or– manually using ground control points

• Alternatives– orbital parameters– ground control points– orthocorrection

• Most accurate results by combining all

Raw image data

• It can be difficult to recognize ground features from raw image data, because they are not necessarily similar than in nature

Raw image vs. corrected image

Geometric correction using orbital parameters

• Information about – position of satellite (XYZ)– attitude ()

• Correction can be low quality due to poor orbital information

• Knowledge about scanning geometry, movement of object and topography (DEM) will increase accuracy


• Accuracy of correction depends on quality of used information

• Some examples about accuracy using orbital parameters:– NOAA AVHRR: 5 km - 1.5 km– Spot 1-4: 350 m– Spot 5: 50 m

• Ground control points: accuracy should be better than 1 pixel– depends also mathematical model and topographic

variations

• Orthocorrection most accurate


Manual correction:• Ground control

points (GCPs): – image

coordinates are measured from image

– map coordinates from map or georeferenced image

Geometric correction• GCPs are known and well distinguished

ground features– crossroads, buildings, small lakes, small

islands, features in waterline

• More GCPs is better• When transformation between image

coordinate system and map coordinate system is defined using polynomials, minimum number of points:– 1st degree polynomial: 3 points– 2nd degree: polynomial: 6 points

Example• Erdas Imagine• Old Landsat TM-image is georeferenced to same

map coordinate system than Landsat ETM-image

Example

• 2nd degree polynomial

• 15 GCPs

Automatic correction• Software searches corresponding points from image

to be georeferenced and image in map coordinate system

• This can be based on– correlation between subimages– recognizable features (linear like roads or lakes)

• These points are used as GCPs• Software produces many (e.g. 200-300 points for

Landsat ETM-image)– user has to select which can be used

• Automatization is needed when there are many images and/or it has to be made daily

Topographic error

• Property of imaging system using central projection

• Image of object is in incorrect place due to height variations

Orthocorrection

• Topographic error is removed by changing the perspective of image from central projection to orthogonal projection

• DEM is needed

Interpolation of digital numbers

• Digital numbers for pixels of corrected image must be interpolated from uncorrected image

• Seldomly number from uncorrected image can be used directly

• Methods– nearest neighbor interpolation– bilinear interpolation– cubic convolution interpolation

Nearest neighbor interpolation

• Take value of closest pixel from uncorrected image

• Easy to compute• Values do not

change• Result can be

inaccurate

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Nearest neighbor interpolation

• Values of some pixels are chosen more than once, some not at all

• ”Piecewise” image

• Linear features can disappear

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Bilinear interpolation

• 4 closest pixels from uncorrected image are used

• Average weighted by distance

• Changes digital numbers– corresponds to average

filtering

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Cubic convolution

• 16 (4x4) closest pixels from uncorrected image are used

• Smaller interpolation error than NN or BL-interpolation

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Image formation• Scene f(x)• Acquired image

g(x)• Scene f(x) is

corrupted by atmosphere and instrument in imaging process

• They act like filters h(x)

Image formation• Image acquisition can be modelled with image

degradation model:

f(x) * h(x) + n(x) = g(x)

g(x): acquired imageh(x): filter corresponding to averaging effects due to

atmosphere and instrumentn(x): random errors due to instrument and data

transmissionf(x): scene

Inverse filtering• Errorness image of scene f(x) should be acquired by

making inverse process to known image g(x)• Image degradation model in frequency domain:

G(u)=F(u)H(u)+N(u)• Ideal inverse filtering

Fe(u) = G(u)/H(u) - N(u)/H(u)

• In practice difficult to solve– zeros in H(u)

– effect of N(u) increases

• Usually radiometric correction is divided to different phases which are corrected individually

Radiometric correction

• In order that measurements taken with– different instruments– differents dates

are comparable

• Aim: radiance or reflectance

• Radiance (W/m2/sr): – physical term which describes intensity of radiation

leaving ground to some direction

• Reflectance: – Radiance / incoming irradiance

Instrument calibration

• Instruments are calibrated before satellite launch– measurements of known targets– instrument response is followed by measuring

calibration targets in instrument or stable targets on ground

• Each channel have calibration coefficients GAIN and OFFSET– these can vary within time– response decreases, so same target looks more dark

Instrument gain

• Pixel digital number is multiplied with gain

radiance = Dn * Gain • Gain = Lmax – Lmin / 255

– Lmax: largest radiance which can be measured by instrument

– Lmin: smallest radiance which can be measured by instrument

Instrument offset

• Background noide detected by instrument

• Measurement, when instrument do not receive any radiation = Lmin

Radiometric correction

• Equation:

R = (Lmax-Lmin)/255*DN + Lmin

OR

R=Gain*DN + offset

Other corrections

• Sun zenith angle:

DN’=DN / SIN(sun)

• Ground is illuminated differently when Sun zenith angle changes– seasonal differences

Other corrections :• Distance between Sun and Earth• This distance varies according to seasons• Irradiance incoming to ground is when taking sun

zenith angle into account:

Atmospheric correction

• Absorption and scattering

• Decrease of diffuse skylight– due to atmospheric scattering– largest at smaller waveleghts (blue), decreases

as wavelenght increases– dampens image contrast


• REF: reflectance of pixel• Lsat: radiance measured by instrument• Lhaze: radiance due to atmospheric scattering (diffuse skylight)• TAUv: atmospheric transmittance from ground to instrument• E0: Sun spectral irradiance outside atmosphere, including effect

of distance between Sun and Earth: E0 = E / d2, where E is Sun spectral irradiance outside atmosphere and d is distance between Sun and Earth in Astronomical Units

• sz: Sun zenith angle• TAUz: atmospheric transmittance from Sun to ground• Edown: maanpinnalle tullut ilmakehän sironnan vaikutus

R E FL L

T A U E C O S sz T A U ESA T H A Z E

V Z D O W N

( )

( )0

Atmospheric correctionApparent reflectance model

• Removes effects of changing Sun-Earth distance and Sun zenith angle

• changing imaging geometry

• Does not remove atmospheric effects: absorption or scattering

• Following parameters for correction model:

TAUz: 1.0, TAUv: 1.0, Edown: 0.0, Lhaze: 0.0

R E FL

E C O S szSA T

( )

( )0

Atmospheric correctionDARK-OBJECT-SUBTRACTION• It is supposed that there are areas in image that are on shadow, so that all

radiation coming to instrument from these areas is due to diffuse skylight• Following parameters for correction model :

TAUz: 1.0

TAUv: 1.0

Edown: 0.0

Lhaze: measure radiance from target which is in shadow (like shadow of cloud) or does not reflect radiation (water in infrared)

R E FL L

E C O S szSA T H A Z E

( )

( )0

Atmospheric correctionCHAVEZ• Modified DOS• Atmospheric transmittances are approximated by angles

of imaging geometry• Following parameters for correction model :

TAUz: cos(sz)

TAUv: 1.0 or cos(incidence angle)

Edown: 0.0

Lhaze: measure radiance from target which is in shadow (like shadow of cloud) or does not reflect radiation (water in infrared)


• More theoretic methods try to model how radiation travels in atmosphere

• Aim is to model – atmospheric transmittance and absorption

– scattering due to gases

– reflectances due to atmosphere, not ground

• Difficult, requires lot of computing and precise knowledge about the state of atmosphere

VTT atmospheric correction• SMAC: Simplified Method of Atmospheric Correction

• Removes Rayleigh scattering, absorption due to atmospheric gases, imaging geometry (sun anlges and distance)

• Digital number reflectance

• Needed

calibration coefficients of instrument

sun zenith and azimuth angles

amount of water vapour

ozone

atmospheric optical depth

VTT atmospheric correction• Original

Landsat ETM-images

• Atmospheric optical Depth can be estimated from image if there are suitable channels

• ETM7/ETM3 ratio should be about 0.4 for olf coniferous forests

VTT atmospheric correction• Corrected

Landsat ETM-mosaic

• Eastern Finland

• 7 images

• RGB: 321

VTT atmospheric correction

Landsat ETM-mosaic of Northern Finland consists of 9 images

Dehazing image• Based on Tasselled Cap-transformation

– TC4 image sensiive to atmospheric effects

• Landsat-5 TM-image:

TC4 = 0.8461*TM1 - 0.7031*TM2 - 0.4640*TM3 - 0.0032*TM4 - 0.0492*TM5 - 0.0119*TM7 + 0.7879

• Image channel is corrected by subtracting TC4 from it

TMcx = TMx - (TC4 - TC40)*Ax

TMcx: Corrected digital number of channel x

TMx: Original digital number of channel x

TC40: Value of haze-free pixel in TC4

Ax: Correction factor determined from image

Dehazing image• Original and corrected TM1

Clouds and their shadows• It is difficult to automatically remove clouds at visible and infrared

regions– thermal infrared helps– thich clouds easy, thin clouds and haze difficult

• Removal by masking– Cloud interpretation Mark their area as ”Nodata” or 0

• Problem shadows– mixed with water areas– difficult to automate

• Relatively simple way:– interprete clouds using thresholding or clustering– make cloud mask (1: cloud, 0: other)– dilate mask– move mask so that it covers also shadows

Topographic correction• Imaging geometry (positions and angles between instrument,

object and radiation source) changes locally

• E.g. deciduous forest on the sunny side or same side as instrument of the hill looks brighter than similar forest on the shadow side

• Reflectance is highest when slope is perpendicular to incoming radiation

Topographic correction

• Correction of image pixel values is based on topographic variations, other characteristics are not taken into account

• Determine the angle between incoming radiation and local surface normal Illumination image cos(i)

Topographic correction• Landsat ETM (RGB: 743) and DEM from NLS

Topographic correction• Landsat ETM (RGB: 743) and illumination image

Topographic correctionVariables of equations:• LO: Original reflectance• LC: Corrected reflectance• sz: Sun zenith angle• i: Angle between incoming radiation and local surface

normal• k: Minnaert coefficient, estimated from image• m: Slope of regression line between illumination image

and image pixels, estimated from image• b: Offset of regression line between illumination image

and image pixels, estimated from image• C: Correction factor of C-correction, C = b/m

Topographic correction• Lambert cosine correction: it is assumed that ground reflects

radiation as Lambertian surface, in other words same amount to different directions

LC = LO COS(sz) / COS(i)

Topographic correction• Minnaert correction: Coefficient k is used to model the effect of

different surfaces

LC = LO [ COS(sz) / COS(i) ]k

Topographic correction• Ekstrand correction: Minnaert coefficient k varies

according to illumination

LC = LO [ COS(sz) / COS(i) ]k COS(i)

Topographic correction• Statistical-empirical correction: correction removes correlation

between illumination image and image channel

LC = LO – m cos(i)

Topographic correction• C-correction: coefficient C should model diffuse light

LC = LO [ ( cos(sz) + C ) / ( cos(i) + C ) ]

ATCOR 2/3• Developed by DLR (German Aerospace Center)

– http://www.op.dlr.de/atcor/

• ATCOR 2/3 tries to remove components 1 and 3:

1. path radiance: radiation scattered by the atmosphere

2. reflected radiation from the viewed pixel

3. radiation reflected by the neighborhood and scattered into the view direction (adjacency effect)

– Only 2 contains information from the viewed pixel.

http://www.op.dlr.de/atcor/

ATCOR 2/3Atmospheric Database• Atmospheres with different vertical profiles of pressure, air

temperature, humidity, ozone content • Various aerosol types (rural, urban, maritime, desert)• Visibilities: 5 - 120 km (hazy to very clear)• Ground elevations 0 - 2.5 km, extrapolated for higher regions• Solar zenith angles 0 - 70 degree• Tilt geometries with tilt angles up 50 degrees are supported• A discrete set of relative azimuth angles (0 - 180 deg., increment 30

deg.) is provided for the atmospheric LUTs of tilt sensors, interpolation is applied if necessary

• Capability for mixing of atmospheres (water vapor, aerosol) • The sensor-specific database is available for the standard

multispectral sensors, i.e., Landsat TM, ETM+, SPOT, IRS-P6 etc.

ATCOR 2• Atmospheric correction for flat terrain• SPECTRA module to determine the atmospheric parameters (aerosol type, visibility,

water vapor)• compare retrieved scene reflectance spectra of various surface covers with library

spectra• tune correction of retrieved spectra so that resemples library spectra• Constant atmospheric conditions or spatially varying aerosol conditions• Retrieval of atmospheric water vapor column for sensors with water vapor bands

(around 940/1130 nm). Example sensors: MOS-B, Hyperion.• Statistical haze removal: a fully automatic algorithm that masks haze and cloud regions

and removes haze of land areas.• De-shadowing of cloud or building shadow areas.• Automatic classification of spectral surface reflectance (program SPECL2) using 10

surface cover templates. This is not a land use classification, but a reflectance-shape classification. Still it may be useful as it is a fast automatic classification algorithm.

• Surface emissivity and surface (brightness) temperature maps for thermal band sensors.• Value added products: vegetation index SAVI, LAI, FPAR, wavelength-integrated

albedo, absorbed solar radiation flux, surface energy fluxes for thermal band sensors: net radiation, ground heat flux, latent heat, sensible heat flux

ATCOR 2Atmospheric correction for flat terrain

• SPECTRA module to determine the atmospheric parameters (aerosol type, visibility, water vapor)– compare retrieved scene reflectance spectra of various surface covers with

library spectra

– tune correction of retrieved spectra so that resemples library spectra

• Constant atmospheric conditions or spatially varying aerosol conditions

• Retrieval of atmospheric water vapor column for sensors with water vapor bands (around 940/1130 nm). Example sensors: MOS-B, Hyperion.

• Statistical haze removal: a fully automatic algorithm that masks haze and cloud regions and removes haze of land areas.

ATCOR 2

• De-shadowing of cloud or building shadow areas.

• Automatic classification of spectral surface reflectance (program SPECL2) using 10 surface cover templates– not a land use classification, but a reflectance-shape classification

• Surface emissivity and surface (brightness) temperature maps for thermal band sensors.

• Value added products: – vegetation index SAVI

– LAI, FPAR

– wavelength-integrated albedo

– absorbed solar radiation flux

– surface energy fluxes for thermal band sensors: net radiation, ground heat flux, latent heat, sensible heat flux

ATCOR 2• examples of haze

removal

IRS-1C Liss-3 scene recorded 25 June 1998 (Craux, France)

Ikonos scene of Dresden, 18 August 2002

ATCOR 2• Dresden, the SPOT-3 sensor (22 April 1995)• Left: surface reflectance after atmospheric correction

(RGB=SPOT bands 3/2/1, NIR/Red/Green)• Right: the results of the automatic spectral reflectance

classificationColor coding of the classification map: - dark to bright green: different vegetation covers - blue: water - brown: bare soil - grey: asphalt, dark sand/soil - white: bright sand/soil - red: mixed vegetation/soil - yellow: sun flower, rape, while blooming

ATCOR 3Correction for mountaineous regions• Scene has to be ortho-rectified• Processing eliminates the atmospheric / topographic

effects and generates surface data (reflectance, temperature) corresponding to a flat terrain

• Features as ATCOR2, except– Quick topographic correction (without atmospheric correction)

– SKYVIEW: sky view factor calculation with a ray tracing program to determine the proportion of the sky hemisphere visible for each pixel of the terrain.

– SHADOW: cast shadow calculation depending on solar zenith and azimuth angle employing a ray tracing program

ATCOR 3• Components:

1. path radiance: radiation scattered by the atmosphere (photons without ground contact)

2. reflected radiation from the viewed pixel

3. adjacency radiation: ground reflected from the neighborhood and scattered into the view direction

4. terrain radiation reflected to the pixel (from opposite hills, according to the terrain view factor)

• Only component 2 contains information from the viewed pixel.

ATCOR 3• Top left: DEM (800 - 1800

m asl)

• Top right: illumination image

• Bottom left: original TM data (bands 3/2/1 coded RGB)

• Bottom right: surface reflectance image after combined atmospheric and topographic correction

• Areas that appear dark in the original image due to a low solar illumination are raised to the proper reflectance level in the corrected image

Walchensee lake and surrounding mountains in the Bavarian AlpsTM scene acquired 28 July 1988

ATCOR 2/3Output:• Surface reflectance channels• Surface (brightness) temperature, surface emissivity map• Visibility index map (corresponds to total optical

thickness at 550 nm) and aerosol optical thickness map• Water vapor map (if required water vapor channels are

available, e.g. at 940 nm)• Surface cover map derived from template surface

reflectance spectra (10 classes): a fast automatic spectral classification.

• Value added channels: SAVI, LAI, FPAR, albedo, radiation and heat fluxes

Errors in images

• Errorneous pixel or scanning lines are due to instrument or data transmission malfunctions

• Fill with neighboring data– bad idea

• Treat as clouds– holes in data

Errors in images• Landsat TM 189/18, 27.7.1989

Errors in images: striping

• Instrument channels have many sensors which are badly calibrated

Errors in images:striping

• IRS WiFS 36/22, 13.6.1999, channel 1 (red)

• Jun 29 1999

Something wrong with data transmission?

Interactive restoration• Interactive restoration of image using Fourier-

transformation

maa-57.2040 kaukokartoituksen yleiskurssi general remote sensing image restoration

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