50 Years of Spaceflight with Fourier Transform Spectrometers (FTS) Built at NASA GSFC

Over the past 50 years, NASA Goddard Space Flight Center (GSFC) has been developing, building, testing and flying a series of Fourier Transform Spectrometers (FTS). This began with the IRIS instruments on the Earth-orbiting Nimbus satellites and progressed to more sophisticated designs optimized for interplanetary spacecraft sent to Mars and later to the outer solar system. Adaptions have been made over time, including progressively higher spectral resolution, sensitivity, numbers of detectors and complexity. Instrument operating temperatures have decreased to enable remote sensing of the cold giant planet systems. In this paper we describe the historical evolution of this instrument line, comparing and contrasting different aspects such as optical design and materials, detector types and data handling. We conclude by looking towards the future. At present the CIRS-Lite prototype is being tested at NASA GSFC for potential use on a future mission to the ice giants, Uranus and Neptune. Surpassing the previous performance of the Voyager IRIS instruments remains challenging, and new technologies that could enable these measurements are discussed

MgB2 Thin-Film Bolometer for Applications in Far-Infrared Instruments on Future Planetary Missions

A SiN membrane based MgB2 thin-film bolometer, with a non-optimized absorber, has been fabricated that shows an electrical noise equivalent power of 256 fW/square root Hz operating at 30 Hz in the 8.5 - 12.35 micron spectral bandpass. This value corresponds to an electrical specific detectivity of 7.6 x 10(exp 10) cm square root Hz/W. The bolometer shows a measured blackbody (optical) specific detectivity of 8.8 x 10(exp 9) cm square root Hz/W, with a responsivity of 701.5 kV/W and a first-order time constant of 5.2 ms. It is predicted that with the inclusion of a gold black absorber that a blackbody specific detectivity of 6.4 x 10(exp 10) cm/square root Hz/W at an operational frequency of 10 Hz, can be realized for integration into future planetary exploration instrumentation where high sensitivity is required in the 17 - 250 micron spectral wavelength range

CIRS-lite, a Fourier Transform Spectrometer for Low-Cost Planetary Missions

Passive spectroscopic remote sensing of planetary atmospheres and surfaces in the thermal infrared is a powerful tool for obtaining information about surface and atmospheric temperatures, composition, and dynamics (via the thermal wind equation). Due to its broad spectral coverage, the Fourier transform spectrometer (FTS) is particularly suited to the exploration and discovery of molecular species. NASA's Goddard Space Flight Center (GSFC) developed the CIRS (Composite Infrared Spectrometer) FTS for the NASA/ESA Cassini mission to the Saturnian system. CIRS observes Saturn, Titan, icy moons such as Enceladus, and the rings in thermal self-emission over the spectral range of 7 to 1000 ell11. CIRS has given us important new insights into stratospheric composition and jets on Jupiter and Saturn, the cryo-geyser and thermal stripes on Enceladus, and the winter polar vortex on Titan. CIRS has a mass of 43 kg, contrasted with the earlier GSFC FTS, pre-Voyager IRIS (14 kg). Future low-cost planetary missions will have very tight constraints on science payload mass, thus we must endeavor to return to IRIS-level mass while maintaining CIRS-level science capabilities ("do more with less"). CIRS-lite achieves this by pursuing: a) more sensitive infrared detectors (high Tc superconductor) to enable smaller optics. b) changed long wavelength limit from 1000 to 300 microns to reduce diffraction by smaller optics. c) CVD (chemical vapor deposition) diamond beam-splitter for broad spectral coverage. d) single FTS architecture instead of a dual FTS architecture. e) novel materials, such as single crystal silicon for the input telescope primary

Thermal Infrared Spectroscopy of Saturn and Titan from Cassini

The Cassini spacecraft completed its nominal mission at Saturn in 2008 and began its extended mission. Cassini carries the Composite Infrared Spectrometer (CIRS); a Fourier transform spectrometer that measures the composition, thermal structure and dynamics of the atmospheres of Saturn and Titan, and also the temperatures of other moons and the rings

Limb Sounding of the Lunar Limb with a Fourier Transform Spectrometer

No abstract availabl

High T(sub c) Superconducting Bolometer on Chemically Etched 7 Micrometer Thick Sapphire

A transition-edge IR detector, using a YBa2Cu3O(7-x) (YBCO) thin film deposited on a chemically etched, 7 micrometer thick sapphire substrate has been built. To our knowledge it is the first such high T(sub c) superconducting (HTS) bolometer on chemically thinned sapphire. The peak optical detectivity obtained is l.2 x 10(exp 10) cmHz(sup 1/2)/W near 4Hz. Result shows that it is possible to obtain high detectivity with thin films on etched sapphire with no processing after the deposition of the YBCO film. We discuss the etching process and its potential for micro-machining sapphire and fabricating 2-dimensional detector arrays with suspended sapphire membranes. A 30 micrometer thick layer of gold black provided IR absorption. Comparison is made with the current state of the art on silicon substrates

STRATOSPHERIC NOxNO_{x} GAS DISTRIBUTIONS FROM BALLOON-BORNE THERMAL EMISSION SPECTRA

Author Institution: Science Systems and Applications, Inc., Seabrook; Department of Physics and Atmospheric Science, Drexel University; Code 693.2, Goddard Space Flight Center, Greenbelt; Department of Physics, University of Denver; code 610.0, Goddard Space Flight Center. , University of Denver; National Center for Atmospheric Research, University of DenverHigh spectral resolution thermal emission spectra of the Earth's stratosphere have been analyzed to retrieve stratospherc thermal struture and the mixing ratio profiles of several minor constituents in the $NO_{x}$ family. The retrieval techniques include line-by-line spectral calculations with an onion-peeling inversion scheme. The retrieved profiles are compared to other observations and a 1-D photochemical model

LOWER STRATOSPHERIC TRACE CONSTITUENTS FROM A BALLOON-BORNE CRYOGENIC INTERFEROMETER

Author Institution: Code 693.2, Goddard Space Flight Center; Department of Physics and Atmospheric Sciences, Drexel University; Department of Physics, University of Denver; Science Systems and Applications, Inc., Seabrook, Maryland 20706.; Code 610.0, Goddard Space Flight Center.; National Center for Atmospheric Research, P.O. Box 3000The infrared emission from minor constituents in the lower stratosphere has been measured using a balloon-borne cryogenic Fourier spectrometer. A liquid-nitrogen cooled interferometer spectrometer with liquid-helium cooled Si:Ga detectors has recorded selected portions of the thermal emission spectrum from $650-2000 cm^{-1}$ with an apodized resolution $0.03 cm^{-1}$. Species identified to date include $CO_{2}, O_{3}, H_{2}O, CH_{4}, HNO_{3}, N O NO_{2}, NO, ClONO_{2}, CCl_{3}F$, and $CF_{2}Cl_{2}$. A tentative identification of $N_{2}O_{5}$ in the $1230 - 1270 cm^{2-1}$ redion has been made