Title: Image Quality Assessment
1Image Quality Assessment
By Jwan M. Aldoski Geospatial Information
Science Research Center (GISRC), Faculty of
Engineering, Universiti Putra Malaysia, 43400
UPM Serdang, Selangor Darul Ehsan. Malaysia
2Image Quality
- Many remote sensing datasets contain
high-quality, accurate data. Unfortunately,
sometimes error (or noise) is introduced into the
remote sensor data by - the environment (e.g., atmospheric scattering,
cloud), - random or systematic malfunction of the remote
sensing system (e.g., an uncalibrated detector
creates striping), or - improper airborne or ground processing of the
remote sensor data prior to actual data analysis
(e.g., inaccurate analog-to-digital conversion).
3154
155
Cloud
155
160
162
MODIS True 143
163
164
4Cloud in ETM
5Striping Noise and Removal
CPCA
Combined Principle Component Analysis
6Speckle Noise and Removal
Blurred objects and boundary
G-MAP
Gamma Maximum A Posteriori Filter
7Remote sensing sampling theory
- Large samples drawn randomly from natural
populations usually produce a symmetrical
frequency distribution most values are clustered
around some central values, and the frequency of
occurrence declines away from this central point-
bell shaped, and is also called a normal
distribution. - Many statistical tests used in the analysis of
remotely sensed data assume that the brightness
values (DN) recorded in a scene are normally
distributed. - Unfortunately, remotely sensed data may not be
normally distributed and the analyst must be
careful to identify such conditions. In such
instances, nonparametric statistical theory may
be preferred.
8Remote sensing pixel values and statistics
- Many different ways to check the pixel values and
statistics - looking at the frequency of occurrence of
individual brightness values (or digital
number-DN) in the image displayed in a histogram - viewing on a computer monitor individual pixel
brightness values or DN at specific locations or
within a geographic area, - computing univariate descriptive statistics to
determine if there are unusual anomalies in the
image data, and - computing multivariate statistics to determine
the amount of between-band correlation (e.g., to
identify redundancy).
91. Histogram
- A graphic representation of the frequency
distribution of a continuous variable. Rectangles
are drawn in such a way that their bases lie on a
linear scale representing different intervals,
and their heights are proportional to the
frequencies of the values within each of the
intervals
10- Histogram of A Single Band of Landsat TM Data of
Charleston, SC - Metadata of the image
- What is metadata?
- Open water,
- Coastal wetland
- Upland
112. Viewing individual pixel values at specific
locations or within a geographic area
- There are different ways in ENVI to see pixel
values - Cursor location/value
- Special pixel editor
- 3D surface view
123. Univariate descriptive image statistics
- The mode is the value that occurs most frequently
in a distribution and is usually the highest
point on the curve (histogram). It is common,
however, to encounter more than one mode in a
remote sensing dataset. - The median is the value midway in the frequency
distribution. One-half of the area below the
distribution curve is to the right of the median,
and one-half is to the left - The mean is the arithmetic average and is defined
as the sum of all brightness value observations
divided by the number of observations.
13Cont
- Min
- Max
- Variance
- Standard deviation
- Coefficient of variation (CV)
- Skewness
- Kurtosis
- Moment
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15Measures of Distribution (Histogram) Asymmetry
and Peak Sharpness
Skewness is a measure of the asymmetry of a
histogram and is computed using the formula
A perfectly symmetric histogram has a
skewness value of zero. If a distribution has a
long right tail of large values, it is positively
skewed, and if it has a long left tail of small
values, it is negatively skewed.
16Measures of Distribution (Histogram) Asymmetry
and Peak Sharpness
A histogram may be symmetric but have a peak that
is very sharp or one that is subdued when
compared with a perfectly normal distribution. A
perfectly normal distribution (histogram) has
zero kurtosis. The greater the positive kurtosis
value, the sharper the peak in the distribution
when compared with a normal histogram.
Conversely, a negative kurtosis value suggests
that the peak in the histogram is less sharp than
that of a normal distribution. Kurtosis is
computed using the formula
17- In this example Kurtosis does not subtract 3.
- http//www.itl.nist.gov/div898/handbook/eda/sectio
n3/eda35b.htm
18We can use ENVI/IDL to calculate them
- ENVI
- Entire image,
- Using ROI
- Using mask
- examples
- IDL
- examples
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204. Multivariate Image Statistics
- Remote sensing research is often concerned with
the measurement of how much radiant flux is
reflected or emitted from an object in more than
one band. It is useful to compute multivariate
statistical measures such as covariance and
correlation among the several bands to determine
how the measurements covary. Later it will be
shown that variancecovariance and correlation
matrices are used in remote sensing principal
components analysis (PCA), feature selection,
classification and accuracy assessment.
21Covariance
- The different remote-sensing-derived spectral
measurements for each pixel often change together
in some predictable fashion. If there is no
relationship between the brightness value in one
band and that of another for a given pixel, the
values are mutually independent that is, an
increase or decrease in one bands brightness
value is not accompanied by a predictable change
in another bands brightness value. Because
spectral measurements of individual pixels may
not be independent, some measure of their mutual
interaction is needed. This measure, called the
covariance, is the joint variation of two
variables about their common mean.
22Correlation
To estimate the degree of interrelation between
variables in a manner not influenced by
measurement units, the correlation coefficient,
is commonly used. The correlation between two
bands of remotely sensed data, rkl, is the ratio
of their covariance (covkl) to the product of
their standard deviations (sksl) thus
If we square the correlation coefficient (rkl),
we obtain the sample coefficient of determination
(r2), which expresses the proportion of the total
variation in the values of band l that can be
accounted for or explained by a linear
relationship with the values of the random
variable band k. Thus a correlation coefficient
(rkl) of 0.70 results in an r2 value of 0.49,
meaning that 49 of the total variation of the
values of band l in the sample is accounted for
by a linear relationship with values of band k.
23example
Pixel Band 1 (green) Band 2 (red) Band 3 (ni) Band 4 (ni)
(1,1) 130 57 180 205
(1,2) 165 35 215 255
(1,3) 100 25 135 195
(1,4) 135 50 200 220
(1,5) 145 65 205 235
Band 1 (Band 1 x Band 2) Band 2
130 7,410 57
165 5,775 35
100 2,500 25
135 6,750 50
145 9,425 65
675 31,860 232
24Band 1 Band 2 Band 3 Band 4
Mean (mk) 135 46.40 187 222
Variance (vark) 562.50 264.80 1007 570
(sk) 23.71 16.27 31.4 23.87
(mink) 100 25 135 195
(maxk) 165 65 215 255
Range (BVr) 65 40 80 60
Univariate statistics
Band 1 Band 2 Band 3 Band 4
Band 1 - - - -
Band 2 0.35 - - -
Band 3 0.95 0.53 - -
Band 4 0.94 0.16 0.87 -
Band 1 Band 2 Band 3 Band 4
Band 1 562.25 - - -
Band 2 135 264.80 - -
Band 3 718.75 275.25 1007.50 -
Band 4 537.50 64 663.75 570
covariance
Correlation coefficient
Covariance
25Feature space plot, or 2D scatter plot in ENVI
- Individual bands of remotely sensed data are
often referred to as features in the pattern
recognition literature. To truly appreciate how
two bands (features) in a remote sensing dataset
covary and if they are correlated or not, it is
often useful to produce a two-band feature space
plot - Demo of 2D scatter plot in ENVI
- Bright areas in the plot represents pixel pairs
that have a high frequency of occurrence in the
images - If correlation is close to 1, then all points
will be almost in 11 lines
26Thank you