A. Trishchenko et Zq. Li, USE OF SCARAB MEASUREMENTS FOR VALIDATING A GOES-BASED TOA RADIATION PRODUCT, Journal of applied meteorology, 37(6), 1998, pp. 591-605
Lack of calibrated radiation measurements at the top of the atmosphere
(TOA) between major spaceborne radiation missions entails inference o
f the TOA radiation budget from operational weather sensors. The infer
red data are subject to uncertainties due to calibration, narrow- to b
roadband conversion, etc. In this study, a surrogate TOA earth radiati
on budget product generated from GOES-7 (Geostationary Operational Env
ironmental Satellite) imagery data for use in the U.S. Atmospheric Rad
iation Measurement (ARM) program was validated using measurements from
the ScaRaB radiometer flown on board the METEOR-3/7 satellite. Compar
isons were made between coincident and collocated shortwave and longwa
ve radiative quantities derived from GOES and ScaRaB sensors over an A
RM experimental locale in the South Great Plains of Oklahoma, during A
pril and July 1994. The comparisons are proven to be instrumental in v
alidating the calibration and narrow- to broadband conversion used to
obtain broadband radiative quantities from GOES digital counts. Calibr
ations for both visible and infrared window channels have small uncert
ainties, whereas narrow- to broadband conversion of shortwave measurem
ents contains large systematic errors. The caveat stems from use of a
quadratic conversion equation instead of a linear one, as was found fr
om ScaRaB narrow- and broadband measurements. The ensuing errors in th
e estimates of broadband albedo depend on scene brightness, underestim
ation for bright scenes, and overestimation for dark scenes. As a resu
lt, the magnitude of the TOA cloud radiative forcing is underestimated
by about 14 W m(-2) or 7.5% on a daytime mean basis. After correcting
this error, the ratio of cloud radiative forcing (a measure of the im
pact of clouds on atmospheric absorption) derived from ARM measurement
s turns out to be 1.07, which is in even closer agreement with radiati
ve transfer models than found from previous studies using original GOE
S products.