Intercomparison of spaceborne microwave radiometers (ERS1-ERS2-TOPEX-SSMI)
Sid-Ahmed Boukabara and Laurence Eymard
CETP, 10-12 avenue de l'Europe 78140 Velizy France
ABSTRACT
Lot of remote sensing applications use simultaneously data obtained from several
satellites instruments. Making maps of geophysical products, validation of radiative
transfer models (by comparing the satellites data to the simulated ones), assimilation
of the remote sensed data in the meteorological prediction models, are some examples
where the synergistic use of the different satellites products is necessary and where
the intercalibration of the measurements is essential (authors like J. Etcheto 1988
underlined this problem). In order to eliminate the differences (and than the errors)
due to the instruments calibration differences, we propose to use an inter-calibration
of these instruments before using their data. The aim is not to change the calibration
of the instruments but to make homogenous the data for the users who need that for
their application. We limited this work to the radiometers only (of ERS-1, ERS-2,
TOPEX-POSEIDON and SSM/I). The work undertaken is based on the cross comparisons
between the different instruments and the comparison with the ECMWF meteorological
fields. We use directly the electromagnetic quantities measured by the instruments
(microwave brightness temperatures MBT) in the different channels (frequency bandwidth:
18 - 85 GHz). First, the intercalibration of these MBT's is done, with a precision
of 1 K. Then, an appropriate retrieval algorithm for each instrument is proposed for
the common retrieved geophysical parameters (integrated water vapour WV, integrated
water content WC and wet tropospheric correction DH). The algorithms are then
validated by comparing their results directly to the coincident on-shipment
measurements. We reach a precision of 1 cm for DH, 0.15 g/cm2 for WV and 2-3 mg/cm2
for WC.
The geophysical products are retrieved using the same algorithms form (linear
logarithmic, described by E. G\'erard, 1996). This permits to get homogenous coverage
when using different remote sensing sources. These algorithms have their own defaults,
but the geophysical data issued from the different satellites will have the same
behaviour. All the data used in this paper are issued from the tandem period where the
four satellites were in orbit (June 1995 to June 1996).
Keywords: ESA European
Space Agency - Agence spatiale europeenne,
observation de la terre, earth observation,
satellite remote sensing,
teledetection, geophysique, altimetrie, radar,
chimique atmospherique, geophysics, altimetry, radar,
atmospheric chemistry
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