In: Wagner W., Székely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Vol. XXXVIII, Part 7B
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Table 1. General specification of the satellite radiometric
systems
Observation geometry of the small satellite system is presented
in Fig. 1. Antenna of the radiometric system will be oriented for
observation in nadir direction and provide spatial resolution
about 350 km and swath width 700 km. In the main operational
mode two beams of the system oriented across the flight
direction in order to have wider swath width. In addition to this
mode it may be possible to rotate the satellite so that two beams
will be in a flight plane. This mode may be useful for
calibration purposes and development of RFI suppression
algorithms.
Fig.l. Observation geometry of the small satellite microwave
system
Advanced L-band radiometric system (ALRS) will be installed
on the module of Russian segment of International Space
Station (RS ISS) (planed installation - 2010). General
specification of the instrument is presented in the last column of
Table 1. It is a set of radiometers with pushbroom 8 beams
antenna. Each beam will have spatial resolution about 50 km.
Observation geometry of the advanced microwave system is
presented in Fig. 2.
Due to relatively large size of the ALRS antenna and
requirements to deliver instrument in compact state through the
manhole it has folding elements and will be deployed manually.
General view of L-band radiometric system in compact
(transport) state is shown in Fig. 3.
Now both radiometric systems are made in technological
versions and are in the procedure of laboratory testing. Results
of testing are in a good agreement with technical requirements.
350450 km
Fig.2. Observation geometry of the advanced microwave
system
Fig.3. L-band radiometric system ALRS in compact (transport)
state.
3. SCIENTIFIC OBJECTIVES AND GENERAL
FEATURES OF THE EXPERIMENTS
Microwave radiometers despite their low spatial resolution are
widely used in space remote sensing of environment. It is due
to ability of microwave radiometry to get data which are
impossible or at least very difficult to get by any other means.
Such data are data on averaged by surface and/or depth
thermodynamic temperature of physical objects, their integral