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Forschungszentrum Karlsruhe Technik und Umwelt C. E. Blom, T. Gulde, C. Keim, W. Kimmig, C. Piesch, C. Sartorius, H. Fischer Institut für Meteorologie und Klimaforschung Forschungszentrum Karlsruhe GmbH / Universität Karlsruhe MIPAS-STR: a new instrument for stratospheric aircraft MIPAS-STR (Michelson Interferometer for Passive Atmospheric Sounding - STRatospheric aircraft) is a new instrument developed for remote sensing of a large number of atmospheric trace compounds (e.g. ClONO2, N2O5, NO, NO2 and HNO3) from high-altitude aircraft. It will be operated from the Russian M-55 Geophysica in the framework of the APE-GAIA (Airborne Polar Experiment Geophysica Aircraft In Antarctica) in September/October 1999. We used modules of the Giessen diode laser system to test Brault’s approach of time-equidistant sampling which was implemented in the electronics of the interferometer of MIPAS-STR. Components of the optic module Scan unit: For accurate pointing and to correct for roll-angle movements of the M55, the scan mirror is continuously adjusted based on the data measured by the instrumentfixed AHRS (Attitude and Heading Reference System). 3-Mirror telescope for stray light suppression. DPI: Interferometer based on the double pendulum principle but with equidistant sampling in the time domain. Cooling system: In order to reduce the background radiation and improve NESR, the optic module is cooled to 200 K. Detector unit: see Figure 3. Line of sight stability Optical path difference (2-sided) Spectral resolution (unapodized) Beam diameter inside the DPI Etendue Scan velocity Detector type (area) Field of view, FOV Signal frequencies 1 arcmin (3) 15 cm 0.034 cm-1 50 mm 2.6 10-3 cm2 sr 3 cm/s Si:As (BIB) (1.6 1.6 mm2) 0.44 (full cone) 2.3 - 5.8 kHz Noise equivalent spectra radiance (NESR): - channel 1: 770 - 1000 cm-1 (13.0 - 10.0 m) - channel 2: 1200 - 1370 cm-1 (8.3 - 7.3 m) - channel 3: 1585 - 1645 cm-1 (6.3 - 6.1 m) - channel 4: 1845 - 1940 cm-1 (5.2 - 5.4 m) Temperature and emissivity of blackbodies: BB1 in the optic module BB2 in the upper isolation of the optics module Accuracy of calibration Sampling frequency (time-equidistant) Sampling frequency (interpolated to equidistant sampling positions) Data rate (4 channels incl. HK data) Refill intervals of cryogenics (lHe, lN2, dry-ice) Electrical power (voltage) Mass (optic module + electronics) [nW/(cm2 sr cm-1] 25 11 3 2 Fig. 1: Artist’s view of the optic module. To reduce size of the instrument the optics is divided in two levels: the upper level contains the scan unit and the telescope, the lower level the interferometer. Fig. 2: Linear representation of the optical path. The IR-radiation propagates from the scan mirror via the telescope and the interferometer to the detector unit. The instrumental FOV is defined by the lHe cooled apertures FS3 and AS3. The apertures AS, FS1 and shields reduce the radiation from outside the FOV as well as scattered radiation reaching the front optics. The radiation diffracted at the edges of the front optics is suppressed by the Lyot and aperture FS2. Fig. 3: The detector system. The entire focal plane with dichroic beam splitters, optical filters, Si:As-detectors etc. is cooled to 4 K. The division into 4 channels is necessary for NESR improvement to facilitate the detection of NO2 and NO (channels 3 and 4) and allows an efficient data reduction. 78 K / 200 K, 0.997 (cavity) about 240 K (floating), 0.98 (plate) 1-3% 48.8 kHz (50 MHz / 1024) 47.4 kHz 50 kB/s 20 h 300 W (28 VDC) 200 kg (150 kg + 50 kg) external PC's Ethernet main control unit - expert system - data storage Table 1: Characteristic instrument data. Onboard electronics and system operation transputer interferometer electronics pilot control panel aircraft avionics link housekeeping and auxiliary electronics line-of-sight electronics AHRS/GPS angle encoder interferometer drive IR data acquisition Main computer: rugged PC with standard interface 14 Unix operating system 12 Transputer network for communication with subsystems Ethernet for connection to the ground station Phase [ °] relay, reset shutter drive housekeeping data pointing mirror drive Fig. 5: Results from blackbody measurements with scan velocities between 1.58 cm/s and 4.30 cm/s. The mean of the phase spectra for forward and backward scans shows the electrical contributions to the phase. 10 8 6 Ground station 4 1000 has access to the main computer and all subsystems transfers the measurement program before take-off allows on-line visualization of all parameters and transfer of data stored during the flight Fig. 4: Scheme of the onboard electronics. The electronics is structured hierarchically. A transputer network connects the central computer with the independent subsystems. The state of the systems is defined by housekeeping and status data. Access from the main computer enables full control during operation of the instrument. 1500 2000 2500 3000 3500 Frequency [Hz] 4000 4500 Fig. 6a: Spectrum of the diode laser. Low current was applied to the TDL to obtain almost monochromatic radiation. The new sampling technique Problem: Vibrations of the aircraft produce perturbations of the scan velocity of the interferometer. If laser fringes establish the sampling positions and a time delay between the laser signal and the IR-interferogram exists, the velocity variations lead to sampling errors and the resulting spectra show phase ghosts or sidebands. Solution: Brault’s approach of time-equidistant sampling was implemented in the Interferometer electronics. Test: Use of Giessen TDL as monochromatic source. Fig. 5: The aircraft M-55 Geophysica. Left: in Pratica di Mare (November 1996). Right: drawing of the M-55 with the ‘dorsal bay’ for MIPAS on top. Fig. 6b: Same as fig. 6b but with expanded vertical scale. Since no monochromator was used, weak secondary lines (below 1%) can be observed. Fig 6c: Spectrum obtained by sine modulating the scan velocity. The modulation frequency was set to 150 Hz, the amplitude (p-p) was 40% of the nominal value of 3 cm/s. A time delay of 0 s was used. Fig 6d: Same as fig. 6c but with time delay of 22 s derived from the phase spectra shown in fig. 5. Note that the ghosts are reduced to about 20%. The non-vanishing part of the ghosts may be due to simultaneous amplitude modulation at the same frequency. August 1999