Zj. Wu et B. Mcavaney, SIMULATION OF IMPACTS OF CLIMATOLOGICAL MSU DATA-PROCESSING METHODS USING NCEP NCAR REANALYSIS DATA/, J GEO RES-A, 103(D16), 1998, pp. 19495-19508
The Microwave Sounding Units (MSUs) aboard TIROS-N/NOAA satellites hav
e played an important role in providing long-term global climate :info
rmation. However, mainly due to the ''limb-correction'' and the ''intr
ascan averaging'' procedures in the data processing, changes to the ch
aracteristics of the data may have occurred. In this paper we investig
ate this possibility in two parts. In the first part we have chosen to
revisit the radiative transfer theory and to re-derive the (effective
) radiative transfer equation for the processed MSU data under more ge
neral conditions. We find that the weighting function of the processed
MSU deviates from the original at nadir and that the normalization co
ndition, which ensures the total weight of contributions to the total
observed radiance from different sources sums up to unity, is breached
. In the later part of the paper we generate simulations of climatolog
ical MSU-2 before and after data processing using a line-by-line radia
tive transfer code of Shah and Rind [1995] with the monthly mean outpu
t of the National Centers for Environmental Prediction (NCEP)/National
Center for Atmospheric Research (NCAR) reanalysis project [Kalnay et
rrl., 1996] for the period 1982-1994. These simulations are examined a
nd compared with the processed MSU-2 observations available in the pub
lic domain. We find that a systematic reduction of contrast between la
nd and ocean MSU-2 brightness temperatures can result from the limb-co
rrection procedure. The temporal variances are affected by the greater
-than-unity limb-correction coefficients, especially in the tropical r
egion. A reduction of the spatial variances over the land region, as w
as reported earlier by Basist et al. [1995], can be caused by the intr
ascan averaging treatment in the processing. We suggest that a better
approach in future MSU data processing may be to use the nadir data di
rectly without averaging with the other off nadir data and, in additio
n, that the off-nadir data should be ''navigated'' and be processed in
to separate data sets.