| ALd ©
Pr ESUN,,.cos6,
Where,
py Unitless planetary reflectance
L , = Spectral radiance at the sensor's aperture
d = Earth-Sun distance in astronomical units from
nautical handbook
ESUN 4" Mean solar Exoatmospheric irradiances
0. = Solar zenith angle in degrees
iii) Estimation of NDVI: Normalized Difference Vegetation
Index (NDVI) was estimated using the following equation
(Hansen et al, 2000):
NDVI = (NIR - Red) (7)
(NIR + Red)
Where,
NIR: Near Infra-Red band
Red: Red band
For Landsat TM and Landsat ETM+ and ALOS AVNIR-2,
band 3 is Red and band 4 is NIR.
3.2.2 Separating Vegetation and Non-vegetation Area:
NDVI threshold was used for grossly separation of vegetation
vs. non-vegetation areas. Furthermore, threshold to NDVI and
then to band 3 brightness was applied to divide vegetation area
into two; named as ‘Vegetation A’, and ‘Vegetation B’. This
was useful for separating relatively dense forest land (that is,
Forest (Closed)) which was found synchronized under
‘Vegetation A’.
Landsat ETM+ had no haze and hence for this image, water
body was separated from non-vegetation area at this step using
threshold to NDVI Threshold followed by some editing. The
non-vegetation excluding water body was named as ‘Other
Non-vegetation’ area.
3.2.3 Unsupervised Classification: The Optical TOA
reflectance image was then clipped separately with the
‘Vegetation A’, ‘Vegetation B’ and ‘Other Non-vegetation’
area boundary. These clipped images were run for unsupervised
classification with 20 classes and employing all 4 bands for
ALOS AVNIR-2 and all bands except band 6 for Landsat TM
and Landsat ETM+.
3.2.4 Recoding and compiling LC Classes: After careful
interpretation of the above yielded classes, these recoded to the
appropriate class and then combined together. Lastly, manual
editing was carried out wherever necessary. Settlements were
found more intermingle with other LC classes, relatively more
manual editing was required to extract this LC class.
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B7, 2012
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia
3.3 Accuracy Assessment of LC Results and Change
Analysis
Accuracy assessment was carried out for LC result from the
latest satellite data, ALOS AVNIR-2 employing the field
experience and secondary information. For this, checking was
done for 230 selected points (pixels), which were randomly
selected throughout the scene
LC change analysis was carried out by overlaying the LC result
all three epochs. For comparison purpose, the LC result from
ALOS AVNIR-2 was resampled to 30m in order to match with
other two epochs (Landsat TM and ETM+). Altogether 242
pixels were tracked for change.
4. RESULTS AND DISCUSSION
4.1 Cloud/Shadow and Haze Identification and Removal
As presented in Figure 4, the result of cloud/shadow and haze
removal for ALOS AVNIR-2 has remained very promising. The
result of removing cloud in Landsat 7 ETM+ was also good,
however, some of the pixels were found mis-replaced which
might be because of the wider gap between acquisition date of
Landsat 7 ETM+ and ALOS PALSAR.
The haze removal algorithm also worked well and it removed
haze from all 3 bands; Blue, Green Red (that is, < 800nm).
Haze appears in these bands (Richter, 2011).
Dehazed Image
ALOS AVNIR-2 4,3,2)
original image
3 Cloud, Shadow, and
Figure 4. ALOS AVNIR-2 Cloud/Shadow & Haze Removal
a) ALOS AVNIR-2 with Cloud/Shadow & Haze
b) Haze Area c) Cloud on to Shadow d) Dehazed image
e) ALOS AVNIR-2 after Cloud/Shadow, Haze Removed
The result of removing cloud in Landsat ETM-- was also good,
however, some of the pixels were found mis-replaced which
might be because of the wider gap between acquisition date of
Landsat 7 ETM- and ALOS PALSAR.
4.2 Land Cover Classification and its Change Detection
As presented in Table 1, overall accuracy is 80.9% and among
the classes, Forest Land has less omission as well as
commission errors. These errors for other LC classes, except
Settlements, are relatively higher. This may be because of
similar spectral reflectance for these LC classes that caused