Marco Gabella, Vlatcheslav Kisselev, and Giovanni Perona, "Retrieval of aerosol profile variations from reflected radiation in the oxygen absorption A band," Appl. Opt. 38, 3190-3195 (1999)
Through a Fredholm integral equation of the first kind, aerosol
kernel functions relate the variations in radiance measured by
satellites to the variations in the aerosol extinction profile and thus
permit profile retrieval from radiance measurements by inversion of the
set of radiative transfer equations for various spectral
intervals. Previously [Appl. Opt. 36, 1328
(1997)] the kernel functions were evaluated for the red and
near-infrared spectral regions outside molecular absorption
bands. Here they are computed within the oxygen A band
with 20-cm-1 spectral resolution. It is shown that,
even with such a relatively low spectral resolution, the new set of
kernels is able to provide better information on and improved accuracy
of the retrieved profile.
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Parameters That Characterize Retrieval Scheme Performance
in the Lower Atmosphere (23–50-km Meteorological Range Transition)
As a Function of Available Measurements within the Oxygen Absorption
A Band
Parameters That Characterize Retrieval Scheme Performance
in the Lower Atmosphere (23–50-km Meteorological Range Transition)
As a Function of Measurements Outside Molecular Absorption
Bandsa
From Ref.
2;
14 403, 9434, and 6510
cm-1;
130° and 170°.
Table 3
Parameters That Characterize Retrieval Scheme Performance
in the Lower Atmosphere (23–50-km Meteorological Range Transition)
Mixing Measurements Both Inside and Outside the Oxygen Absorption
A Band
From Ref. 2;
14 403, 12 800, 11 430, 9434, and
6510 cm-1;
130°, 140°,
150°, and 170°.
Tables (5)
Table 1
Parameters That Characterize Retrieval Scheme Performance
in the Lower Atmosphere (23–50-km Meteorological Range Transition)
As a Function of Available Measurements within the Oxygen Absorption
A Band
Parameters That Characterize Retrieval Scheme Performance
in the Lower Atmosphere (23–50-km Meteorological Range Transition)
As a Function of Measurements Outside Molecular Absorption
Bandsa
From Ref.
2;
14 403, 9434, and 6510
cm-1;
130° and 170°.
Table 3
Parameters That Characterize Retrieval Scheme Performance
in the Lower Atmosphere (23–50-km Meteorological Range Transition)
Mixing Measurements Both Inside and Outside the Oxygen Absorption
A Band