Yj. Kaufman et al., THE MODIS 2.1-MU-M CHANNEL - CORRELATION WITH VISIBLE REFLECTANCE FORUSE IN REMOTE-SENSING OF AEROSOL, IEEE transactions on geoscience and remote sensing, 35(5), 1997, pp. 1286-1298
A new technique for remote sensing of aerosol over the land and for at
mospheric correction of Earth imagery is developed, It is based on det
ection of dark surface targets in the blue and red channels, as in pre
vious methods, but uses the 2.1-mu m channel, instead of the 3.75 mu m
for their detection, ii 2.1-mu m channel is present on ADEOS OCTS and
GLI, and planned on EOS-MODIS and EOSP, and a similar 2.2-mu m channe
l is present on Landsat TM. The advantage of the 2.1-mu m channel over
the 3.75-mu m channel is that it is not affected by emitted radiation
, The 2.1-mu m channel is transparent to most aerosol types (except du
st) and therefore can be used to detect dark surface targets, Correlat
ion between the surface reflection in the blue (0.49 mu m), red (0.66
mu m), and 2.1 mu m is established using atmospherically corrected Lan
dsat TRI and AVIRIS aircraft images collected over the Eastern United
States, Maine, and California and spectral data obtained from the grou
nd and Light aircraft near San Diego, CA. Results from a variety of su
rface covers show that the surface reflectance at 0.49 mu m (rho(0.49)
) and 0.66 mu m (rho(0.66)) can he predicted from that at 2.2 mu m (rh
o(2.2)) within Delta rho = +/-0.006 for rho(2.2) less than or equal to
0.10, using rho(0.49) = rho(2.2)/4 and rho(0.66) = rho(2.2)/2. Error
in surface reflectance of 0.006 corresponds to an error in remote sens
ing of aerosol optical thickness, tau, of Delta tau similar to +/-0.06
. These relationships were validated using spectral data taken close t
o the surface over vegetated areas in a different biome, This method e
xpands application of dark targets for remote sensing of aerosol to br
ighter, nonforested vegetation, The higher reflection of the surface a
t 2.2 mu m than that of 3.75 mu m mag even enable remote sensing of du
st above surfaces with reflectivity rho(2.2) = 0.15 +/- 0.05. For this
reflectivity range the dust radiative effect at 2.2 mu m is small, an
d the surface reflectance in the blue and red channels can be retrieve
d.