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Dr. David H. Atkinson Dept. Electrical & Computer Engineering University of Idaho 8 April 2005 Measuring the Zonal Winds on Titan: The Huygens Probe Doppler Wind Experiment
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Cassini/Huygens
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HST
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Voyager 1
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Transmitter Ultrastable Oscillator (TUSO) Radar Altimeter Antennas GCMS Atmospheric Structure Instrument Descent Imager Surface Science Package Command Data Management Unit (CDMU) Accelerometers
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Batteries PCDU ACP SSP GCMS
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KSC, Cape Canaveral: 15 Oct 1997
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Cassini SOI: 1 July at 02:36 UT
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Christmas Day 2004
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14 January 2005 7 years, 3 months and 4 billion km from launch
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Titan: Pre-Cassini/Huygens N2, CH4, and H2 atmosphere cause a mild greenhouse effect that raises the surface temperature by +21K. High altitude optically thick organic haze absorbs solar visible but is transparent to IR, cooling surface temp by about 9K. (anti-greenhouse effect).
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Huygens’ Scientific Payload ACP - Aerosol Collector and Pyrolyser (G. Israel, France) –Collection of aerosols for chemical-composition analysis. GCMS - Gas Chromatograph and Mass Spectrometer (H. Niemann, NASA GSFC) –gas chemical analyser designed to identify and quantify various atmospheric constituents. DISR - Descent Imager & Spectral Radiometer (M. Tomasko, U. Arizona) –images and spectral measurements. Also spectra of the surface material will be acquired. DWE - Doppler Wind Experiment (M. Bird, U. Bonn) –Wind measurements using Probe/Orbiter radio signal HASI - Huygens Atmosphere Instrument (M. Fulchignoni, Italy) – physical and electrical properties of the Atmosphere SSP - Surface Science Package (J. Zarnecki, UK) –physical properties of the surface at the impact site
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DWE Concept Goal: In situ determination of zonal wind speed along Huygens descent path Approach: Record Doppler effect on Huygens carrier signal => radial velocity Input parameters: 1.Huygens descent speed, meridional speed 2.Huygens starting position 3.Cassini position & velocity
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Ultra-stable Oscillators (USOs) TUSO on Huygens Probe RUSO in Huygens Receiver on Cassini Orbiter DWE Hardware
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No power!
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Channel B Temperature Compensated Crystal Oscillator
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DWE from Earth: Geometry Huygens antenna pointed only ~30° from Earth Better SNR than for Galileo Probe detection at Jupiter Probe velocity projection in direction to Earth nearly antiparallel to projection in direction to Orbiter
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Huygens VLBI Network Facility Start UTCStop UTCComment GBT09:31:1012:15:00 DWE: Real time RSR detection VLBA Fort Davis09:31:1013:45:00 VLBA North Liberty09:31:1013:15:00 VLBA Owens Valley09:30:0914:49:14DWE: No nodding – on Titan continuously VLBA Pie Town09:30:1114:15:04DWE: No nodding – on Titan continuously VLBA Los Alamos09:31:1014:00:00 VLBA Brewster09:31:1014:48:00 VLBA Kitt Peak09:31:1014:15:00DWE VLBA Mauna Kea09:31:1016:00:00DWE Parkes12:26:2316:00:00DWE: Real time RSR detection Hobart11:13:1016:00:00 Ceduna10:13:1016:00:00 Mopra10:10:1016:00:00 Kashima09:31:1016:00:00 Shanghai10:01:1016:00:00 Urumqi11:31:1016:00:00Calibration only, no Huygens signal at 2040 MHz ATCA10:01:1016:00:00Calibration only, no Huygens signal at 2040 MHz Onsala19:01:1022:15:00 Wettzell21:46:1022:15:00
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Parkes Telescope Australia Green Bank Telescope West Virginia
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Huygens Radio Tracking Net 10:18 UTC-ERT12:30 UTC-ERT
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Huygens! (~ -171 dBm) 10:18:15 UTC-GRT10:18:10 UTC-GRT Green Bank Telescope
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Huygens Frequency: GBT + Parkes
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DWE: Preliminary Results Zonal winds above boundary layer are PROGRADE Low-velocity layer between 60-80 km –Stong positive/negative wind shear –‘Unexpected’, but evident in some GCMs Considerable turbulence above 100 km Near surface winds are weak (~ 1-2 m/s)
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Adieu, Huygens
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