Description of a New Method for Retrieving the Aerosol Optical Thickness from Satellite Remotely Sensed Imagery Using the Maximum Contrast Value and Darkest Pixel Approach
Journal
Transactions in GIS
Date Issued
2008
Author(s)
DOI
10.1111/j.1467-9671.2008.01121.x
Abstract
Satellite sensors have provided new datasets for monitoring regional and urban air
quality. Satellite sensors provide comprehensive geospatial information on air quality
with both qualitative remotely sensed imagery and quantitative data, such as aerosol
optical depth which is the basic unknown parameter for any atmospheric correction
method in the pre-processing of satellite imagery. This article presents a new method
for retrieving aerosol optical thickness directly from satellite remotely sensed imagery
for short wavelength bands in which atmospheric scattering is the dominant
contribution to the at-satellite recorded signal. The method is based on the determination
of the aerosol optical thickness through the application of the contrast tool
(maximum contrast value), the radiative transfer calculations and the ‘tracking’ of
the suitable darkest pixel in the scene. The proposed method that needs no a-priori
information has been applied to LANDSAT-5 TM, LANDSAT-7 ETM
+
, SPOT-5 and
IKONOS data of two different geographical areas: West London and Cyprus. The
retrieved aerosol optical thickness values show high correlations with in-situ visibility
data acquired during the satellite overpass. Indeed, for the West London area a
logarithmic regression was fitted for relating the determined aerosol optical thickness
with the in-situ visibility values. A high correlation coefficient (
r
2
=
0.82;
p
=
0.2)
was found. Plots obtained from Tanre et al. (1979, 1990) and Forster (1984) were
reproduced and estimates for these areas were generated with the proposed method
so as to compare the results. The author’s results show good agreement with Forster’s aerosol optical thickness vs. visibility results and a small deviation from Tanre’s
model estimates.
quality. Satellite sensors provide comprehensive geospatial information on air quality
with both qualitative remotely sensed imagery and quantitative data, such as aerosol
optical depth which is the basic unknown parameter for any atmospheric correction
method in the pre-processing of satellite imagery. This article presents a new method
for retrieving aerosol optical thickness directly from satellite remotely sensed imagery
for short wavelength bands in which atmospheric scattering is the dominant
contribution to the at-satellite recorded signal. The method is based on the determination
of the aerosol optical thickness through the application of the contrast tool
(maximum contrast value), the radiative transfer calculations and the ‘tracking’ of
the suitable darkest pixel in the scene. The proposed method that needs no a-priori
information has been applied to LANDSAT-5 TM, LANDSAT-7 ETM
+
, SPOT-5 and
IKONOS data of two different geographical areas: West London and Cyprus. The
retrieved aerosol optical thickness values show high correlations with in-situ visibility
data acquired during the satellite overpass. Indeed, for the West London area a
logarithmic regression was fitted for relating the determined aerosol optical thickness
with the in-situ visibility values. A high correlation coefficient (
r
2
=
0.82;
p
=
0.2)
was found. Plots obtained from Tanre et al. (1979, 1990) and Forster (1984) were
reproduced and estimates for these areas were generated with the proposed method
so as to compare the results. The author’s results show good agreement with Forster’s aerosol optical thickness vs. visibility results and a small deviation from Tanre’s
model estimates.