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    ra nng ourse

    Remote Sensing Basic Theory & Image Processing

    Methods

    Michiel DamenMichiel Damen (September 2011)(September 2011)@@

    ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE

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    Geometric Operations

    Contents

    Two dimensional approaches

    Georeferencing eoco n

    Three dimensional approaches

    Orientation

    Stereo restitution

    Questions

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009

    ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 2

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    Geometric Operations

    Why correct images for geometric

    distortions ?

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009

    ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 3

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    Geometric Operations

    Why correct images for geometric

    distortions ?

    1. To get 2-dimensional (x, y) and 3 dimensional (x,

    ,

    2. To visualize the image data in a GIS environment

    3. To merge (fuse) different types of image data,for instance in a GIS or multi-tem oral anal sis

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 4

    (monitoring)

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    Geometric Operations

    Elementary image distortions

    -

    of geometric image

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 5

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    Geometric Operations

    Elementary image distortions

    images of large scaler

    H

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 6

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    Geometric Operations

    Elementary image distortions

    Enschede

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 7

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    Geometric Operations

    To be used if relief displacement can be neglected:

    Two dimensional approaches

    (1) flat terrain or (2) space imagery with low resolution

    The objective is to relate the image coordinate system to

    a spec cmap

    coor nate systemImage Map

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 8

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    Geometric Operations

    Georeferencing

    1. Selection of the appropriate type oftransformation

    .

    A geometric transformation is a function that

    for instance map x, y to image: i, j

    The t e of transformation to be used de ends mainl

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 9

    on the type of sensor-platform

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    Geometric Operations

    Types of transformation

    rans orma on : correc s or p c an

    roll in for instance aerial photographs

    st nd th, .

    In most situations 1st order adequate

    x = a + bi + cj x, y : map coordinates

    y = d + ei + fj i,j : image coordinates

    The six transformation parameters ( a. f) can be

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 10

    determined by Ground Control Points ( GCPs )

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    Geometric Operations

    Ground Control Points ( GCPs )

    s : po n s acan be clearly identified both in the image and

    in a source with the required map projection.

    Sources: (1) topographical map, (2) alreadyrectified image, (3) GPS field points !

    Master Slave Image Map

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 11

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    Geometric Operations

    Rectification in ERDAS Imagine (image-to-image)

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 12

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    Geometric Operations

    Accuracy of the transformation

    : ca cu a es amean value from the individual residuals, both in x

    and y direction.

    ! Warning !

    The RMS error does not take into account the spatial

    distribution of the GCPs and also not the accuracy of

    the person trying to find the Control Points !!

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 13

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    Geometric Operations

    Accuracy of the transformation

    n

    i

    ix dxn

    m1

    n21

    22)( yxtotal mmRMSEm

    Root Mean Square Error

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 14

    i

    iyn

    m1

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    Geometric Operations

    Images Original and geo-referenced

    Original image Geo-referenced image

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 15

    Flevoland - IJssel delta, The Netherlands Co-ordinates

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    Geometric Operations

    Geocoding -> Resampling

    s geo-re erenc ng w su sequen

    Resampling of the raster image.

    1. Projection of raster onto

    the original image using the

    trans ormat on parameters

    2. Resamplingof raster image

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 16

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    Geometric Operations

    Transformation types for Geo-coding

    ,

    based on their increase in complexity:

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 17

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    Geometric Operations

    Transformation types for Geo-coding

    Conformal (4 parameters):

    Rotation, scaling,

    preservation of angles (shape)

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 18

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    Geometric Operations

    Transformation types for Geo-coding

    Affine (8 parameters):

    Rotation, scaling,

    preservation of parallels

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 19

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    Geometric Operations

    Transformation types for Geo-coding

    Polynomial (2nd order):

    Rotation, scaling,

    no preservation of parallelsstrai ht lines become curved

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 20

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    Geometric Operations

    Resampling types for raster image

    output raster image are different, interpolation is

    required for each pixel.

    Resampling methods:

    Nearest NeighbourNearest Neighbour

    Bilinear Interpolation

    Cubic Interpolation

    Cubic Interpolation

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 21

    Green line original image

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    Geometric Operations

    Resampling types for raster image

    Nearest Neighbour

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 22

    Pixel value(s) retained !

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    Geometric Operations

    Resampling types for raster image

    Bilinear Interpolation

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 23

    Smooth result

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    Geometric Operations

    Choice of resampling types

    Spectral Spatial accuracy

    Nearest neighbour : spectral information retained

    u c n erpo a on : smoo er spa a n orma on

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 24

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    Geometric Operations

    Images Georeferenced vs. Geocoded

    Georeferenced ima e Geocoded ima e

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 25

    Flevoland - IJssel delta, The Netherlands

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    Geometric Operations

    Images Topomap vs . Geocoded image

    To o ra hical ma Geocoded ima e

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 26

    Flevoland - IJssel delta, The Netherlands

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    Geometric Operations

    Three-dimensional approaches (1)

    MonoplottingUsin a DEM to calculate terrain coordinates no re-sam lin

    Ortho-image productionResampling of an image into map geometry taking terrainrelief into account

    Stereo-restitutionUse of two images (stereo-pair) to extract 3D information

    Orietation

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 27

    Results in formula to calculate image coordinates (X, Y) fromterrain coordinates (x, y, z)

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    Geometric Operations

    Three-dimensional approaches (2)

    geospatial data describes the horizontal position of

    terrain features : X, Y coordinates

    displacement

    3D geospatial data also considers also vertical positionof terrain features (for instance height above sea

    level) : X, Y, Z coordinates

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 28

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    Geometric Operations

    Three-dimensional approaches (3)

    the ground surface

    surface, including

    vegetation, infra-

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 29

    , .

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    Geometric Operations

    Three-dimensional approaches (4)

    recons ruc on o e pos on othe projection centre of sensor: AP-> Principal Point

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 30

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    Geometric Operations

    Three-dimensional approaches (5)

    : econs ruc on o pos onand attitude / inclination of the sensor with respect toterrain coordinate system.

    Parameters:

    1. Indirect camera orientation: Measurements of GCP

    in the terrain X Y and Z

    2. Direct camera orientation: Orientation of the

    sensor itself (position and attitude) by GPS and

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 31

    3. Integrated Camera orientation: Combi of 1. and 2.

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    Geometric Operations

    Three-dimensional approaches (6)

    :

    RPC : Rational Polynomial Coefficient

    coordinates of an entire frame and terraincoordinates.

    Can be used by RS software, such as

    ERDAS Imagine

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 32

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    Geometric Operations

    Three-dimensional approaches (7)

    onop o ng: s ng a o ca cu a e erra n

    coordinates no resampling needed

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 33

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    Geometric Operations

    Three-dimensional approaches (8)

    r op o o: esamp ng o an mage n o map

    geometry taking terrain relief into account

    Monoplotting+

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 34

    ResamplingOn the original aerial photo Geometrically correct

    the map grid is distorted orthophoto

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    Geometric Operations

    Three-dimensional approaches (9)

    ereo res u on: se o wo mages s ereo-

    pair) to extract 3D information. For measurements

    use is made of arallax

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 35

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    Geometric Operations

    Summary (1)

    To correct mages 2 mens ona y or stort ons:

    1. Georeferencing

    2. Geocoding

    Use of appropriate Transformation

    Use of Ground Control Points (GCP) from GPS or

    Topographical map

    Transformation types:

    Conformal: preservation of angles

    Affine: reservation of arallels

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 36

    Polynomical (2nd order)

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    Geometric Operations

    Summary (2)

    Image resampling methods:

    Nearest Neighbour : pixel values retained

    Bilinear Inter olation: smooth result

    Cubic convolution Three dimensional approaches for correction of

    Internal & external orientation

    Monoplotting

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 37

    Use of DEM

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    Geometric Operations

    Questions

    INTERNATIONAL INSTITUTE FOR GEO-INFORMATION SCIENCE AND EARTH OBSERVATIONDamen 2009ITC FACULTY OF GEO-INFORMATION SCIENCE AND EARTH OBSERVATION, UNIV. OF TWENTE 38