Instrument Information
|
| IDENTIFIER |
urn:esa:psa:context:instrument:hp.disr::1.2
|
| NAME |
Descent Imager Spectral Radiometer for Huygens Probe
|
| TYPE |
Imager
|
| DESCRIPTION |
The Descent Imager Spectral Radiometer (DISR) on the Huygens Probe was an optical instrument that made measurements at solar wavelengths. Sunlight plays a key role in driving many important physical processes in planetary physics. Absorption of UV light drives photochemical reactions, leading to changes in atmospheric composition and the production of atmospheric aerosols. The size, shape, composition and distribution of aerosols and cloud particles determine their optical properties and their ability to absorb sunlight and emit thermal infrared radiation. Thus they play a key role in the atmosphere's thermal balance. The net radiative heating or cooling rate provides the forcing for atmospheric dynamics, which in turn can affect the distribution of aerosol and cloud particles and influence climate. DISR measured solar radiation using silicon photodiodes, a 2D silicon Charge Coupled Device (CCD) detector and two InGaAs near-IR linear array detectors. Fiber optics connected the detectors to many separate sets of foreoptics that collect light from different directions and in different spectral regions. In this way, the instrument collected a suite of measurements that were carefully selected to answer key questions concerning the nature of Titan's surface and the composition, meteorology, thermal balance and clouds and aerosols in Titan's atmosphere. The composition, thermal balance, dynamics and meteorology of the atmosphere also affect (and are affected by) the nature of the surface. Surface images in reflected sunlight, together with near-IR reflection spectra, can reveal the nature of the surface and its interactions with atmospheric processes. Optical measurements of solar radiation made inside a planetary atmosphere can thus reveal a great deal about many important physical processes occurring there.
|
| MODEL IDENTIFIER |
|
| NAIF INSTRUMENT IDENTIFIER |
|
| SERIAL NUMBER |
not applicable
|
| REFERENCES |
Bodin, P., and J.F. Reulet, A New Channel for SPOT in the SWIR Band. S.P.I.E. 865, 142-149, 1987
Dave, J.V., Determination of size distribution of spherical polydispersions using scattered radiation data. Appl. Opt. 10, 2035-2044, 1971
Hunten, D., M.G. Tomasko, F.M. Flasar, R.E. Samuelson, D.F. Strobel, and Stevenson, D.J., Titan. In Saturn, editors T. Gehrels and M.S. Matthews, pp. 671-759, University of Arizona Press, 1984
Lemmon, M.T., E. Karkoschka, and Tomasko, M., Titan's rotational light curve. Icarus 113, 27-38, 1995
Lunine, J.I., Does Titan have an ocean? A review of current understanding of Titan's surface. Rev. Geophysics 31, 133-149, 1993
Lunine, J., F.M. Flasar, and Allison, M.D., Huygens Probe Wind Drift: Science Issues and Recommendations, A Report to the Huygens Project, 1991
Muhleman, D.O., A.W. Grossman, B.J. Butler, and M.A. Slade, Radar reflectivity of Titan, Science 248, 975, 1990
Nakajima, T., T. Masayuki, and T. Yamauchi, Retrieval of the optical properties of aerosols from aureole and extinction data. Appl. Opt. 22, 2951-2959, 1983
Smith, P.H., M.T. Lemmon, R.D. Lorenz, L.A. Sromovsky, J.J. Caldwell, and M.D. Allison, Titan's Surface, Revealed by HST Imaging, Icarus, Volume 119, Issue 2, pp.336-349., 2/1996.
M.G. Tomasko, L.R. Doose, P.H. Smith, R.A. West, L.A. Soderblom, M. Combes, B. Bezard, A. Coustenis, C. deBergh, E. Lellouch, J. Rosenqvist, O. Saint-Pe, B. Schmitt, Hu. U. Keller, N. Thomas & F. Gliem, The Descent Imager/Specral Radiometer (DISR) Aboard Huygens, Huygens Science Payload and Mission SP-1177:109-138, 1997.
West, R.A., and P.H. Smith, Evidence for aggregate particles in the atmospheres of Titan and Jupiter. Icarus 90, 330-333. 138, 1991
|
|