Microwave radiometry and interferometry of Uranus

Physics

Scientific paper

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Brightness Temperature, Interferometry, Microwave Radiometers, Planetary Atmospheres, Temperature Distribution, Uranus (Planet), Ammonia, High Resolution, Insolation, Planetary Temperature, Synchrotron Radiation, Uranus, Interferometry, Microwave Radiometry, Wavelengths, Models, Brightness Temperature, Emissions, Disk, Ammonia, Opacity, Hydrogen Sulfide, Observations, Flux Density, Phases, Abundance, Radiation Belt, Atmosphere, Gradients, Procedure, Insolation, Vapor Pressure, Heat Source, Polar Regions, Eq

Scientific paper

Results are presented of high-resolution interferometry of Uranus at 6 cm wavelength and single-dish observations of the disk-averaged brightness temperature at 2.8 and 4.8 wavelength. The 1978 brightness temperature measurements support the finding of Klein and Turegano (1978) that the brightness temperature of Uranus has been rising; there is no evidence for radio emission from the outside the visible disk at 6 cm. The interferometry shows a possible 55 plus or minus K difference in brightness temperature between the equator and the currently exposed pole. The changing insolation probably triggers a redistribution of the trace constituent NH3 which is reponsible for radio opacity.

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