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MOPITT Product Quality Summary |
This statement applies to Level 1 Version 1 data (Local Version ID
2.19.3).
October 20, 2000
There has been no previous heritage instrument with which MOPITT can easily be compared. Therefore validation is a challenge. The data released are in the preliminary stages of calibration and validation. Significant improvements are expected as the MOPITT team better characterizes the instrument's in-flight behavior and the validation campaign progresses.
Known problems:
Thermal Channel Filter Shifts
A systematic discrepancy between the expected (i.e. calculated) Average
radiances and the observed radiances was detected (~7%) in the thermal
channels. The source of this discrepancy is believed to be caused by a shift of
the optical filters of a few wavenumbers. The cause of the shift is believed to
be a combination of thermal effects and possibly errors in measuring the filter
position and shape. The magnitude of the shift is being estimated empirically
and corrected for in the processing software. These data are the first attempt
at rectifying this problem. The discrepancy in these data for the thermal
channels has been reduced to less than 1% in the inner pixels. Refinements are
expected.
Inner/Outer Pixel Contrast
MOPITT has an array of four pixels in a line. It appears that the inner two
pixels of the line register slightly higher radiances than the outer two
pixels. This effect is being investigated. Future releases will attempt to
correct this bias.
Solar Channel Filter Shifts
There are known differences between the best estimates of the filter positions
in the 2.2 and 2.3 micron bands and the positions implemented in the processing
software. This is not expected to have a major effect on results, and will be
corrected in future versions.
Solar Channel Radiance Variations
The observations of land (as opposed to ocean) are quite variable over the
course of a MOPITT stare. This may introduce errors that more clever
processing algorithms may reduce or avoid.
Noise Values
Noise values are estimates, rather than calculations based on the data. These
are in the process of being incorporated.
Validation Data
There are no independent observations of MOPITT radiances. Validation
experiments, especially based on the MOPITT-Airborne Simulator (MOPITT-A) which
flew on the NASA ER-2 aircraft during the SAFARI Program in Southern Africa,
are now taking place. Validation is also being carried out through comparison
with calculations based on in situ measurements. The results are slowly being
assimilated by the MOPITT science team. More time is needed to take advantage
of the independent corroborative data.