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Download Looking at our Neighbors with the VLA
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Planetary Radio Astronomy Bryan Butler What kinds of things do we observe with the VLA? 45% - Extragalactic 20% - Galactic 30% - Stellar 5% - Solar system Solar System “Bodies” Sun IPM Giant planets Terrestrial planets Moons Small bodies Planetary Radio Astronomy Observation of radio wavelength radiation which has interacted with a solar system body in any way, and use of the data to deduce information about the body: spin/orbit state surface and subsurface properties atmospheric properties magnetospheric properties ring properties Types of radiation: thermal emission reflected emission (radar or other) synchrotron emission occultations Mercury Closest to Sun Magnetic field No atmosphere Hot! Mercury - Thermal Emission Mitchell & de Pater 1994 The Goldstone/VLA Radar Mercury - Radar Butler et al. 1993 polar ice? Volcanoes? Venus Closest to Earth Thick atmosphere Hot! Venus - models Venus models at C, X, U, and K-bands: Venus - residuals Venus residual images at U and K-bands: Venus – Thermal Emission Examination of the brightness temperature spectrum of Venus shows unexpected behavior at long wavelengths: Moon – scaled & offset Mars Most like Earth Thin atmosphere Cold Interesting Geology Mars - Atmospheric Water Clancy, Grossman, & Muhleman 1992 cold & dry! Mars - Radar Butler, Muhleman & Slade 1994 polar cap lava flows “Stealth” Jupiter Biggest planet Gas ball “weather” (GRS) rings Jupiter - Synchrotron De Pater, Schulz & Brecht 1997 = 20cm 3-D Reconstruction Developed by Bob Sault (ATNF) - see Sault et al. 1997; Leblanc et al. 1997; de Pater & Sault 1998 Saturn 2nd biggest planet Gas ball “weather” Rings Saturn - Thermal Emission van der Tak, de Pater, Silva & Millan 1997 = 2cm Titan Bigger than Pluto thick atmosphere (haze/smog) ice + liquid surface Titan - Radar Muhleman, Grossman, & Butler 1995 no global ethane/ methane ocean maybe ‘seas’?