Microwave Radiometer (Juno)


Microwave Radiometer is an instrument on the Juno orbiter sent to planet Jupiter. MWR is a multi-wavelength microwave radiometer for making observations of Jupiter's deep atmosphere. MWR can observe radiation from 1.37 to 50 cm in wavelength, from 600 MHz to 22 GHz in frequencies. This supports its goal of observing the previously unseen atmospheric features and chemical abundances hundreds of miles/km into Jupiter's atmosphere. MWR is designed to detect six different frequencies in that range using separate antennas.
MWR views Jupiter's microwave radiation so it can see up to hundreds of miles deep into the planet. In August 2016, as Juno swung closely by the planet MWR achieved a penetration of 200 to 250 miles below the surface cloud layer. MWR is designed to make observations below the cloud-tops, especially detecting the abundances of certain chemicals and determine dynamic features. The region has not been observed like this previously.
MWR was launched aboard the Juno spacecraft on August 5, 2011 from Cape Canaveral, USA, as part of the New Frontiers program, and after an interplanetary journey that including a swingby of Earth, entered a polar orbit of Jupiter on July 5, 2016,
The electronics for MWR are located inside the Juno Radiation Vault, which uses titanium to protect it and other spacecraft electronics. The antennas and transmission lines are designed to handle the radiation environment at Jupiter so the instrument can function.

Goals

Determining the features and abundances of oxygen, nitrogen, and sulfur at up to 100 Bars of pressure will shed light on the origins and nature of Jupiter. It is also designed to detect the amount water and ammonia deep inside Jupiter. It should also be able to provide a temperature profile of atmosphere down to 200 bar. Overall MWR is designed to look down as deep as roughly 1,000 atmospheres which is about 342 miles down inside Jupiter.
One of the molecules MR is intended to look for inside Jupiter is water, which it is hoped well help explain the formation of the Solar System. By probing the interior, the insights may reveal how and where Jupiter formed, in turn shedding understanding on the formation of the Earth.
At the time of its use in the 2010s, it was one of only four microwave radiometers to have been flown on interplanetary spacecraft. The first was Mariner 2, which used a microwave instrument to determine the high surface temperature of Venus was coming from the surface not higher up in the atmosphere. There is also radiometer type instruments on Rosetta comet probe, and Cassini-Huygens. Previously, the Galileo probe directly measured Jupiter's atmosphere in situ as it descended into the atmosphere, but only down to 22 bars of pressure. However, MWR is designed to look down as deep as 1000 bar of pressure.

Antennas

MWR has six separate antennas of different size that are mounted to the sides of the Juno spacecraft body. As the spacecraft turns each antenna takes a "swath" of observations of the giant. Five of the six antennas are all on one side of the spacecraft. The sixth and biggest antenna entirely fills another side the Juno body.
MWR antennas: MWR has six antennas on two different sides of Juno There are two patch array antennas, three slot arrays, and one horn antenna.
As Juno turns the antennas sweep across Jupiter, each frequency/wavelength capable of seeing a certain distance below the visible cloud tops.
See also Reflective array antenna and Slot antenna

Results

During a close pass in summer of 2017 when MWR was operated at Jupiter, it detected temperature changes deep within the Great Red Spot storm. On Perijove 7, which was the sixth science orbit MWR took readings of Jupiter's great red storm down to dozens of kilometers/miles of depth below the surface layers.
The distribution of ammonia gas was reported on in 2017, and analyzed. An ammonia rich layer was identified, as well as a belt of ammonia poor atmosphere from 5 to 20 degrees north.
During the first eight orbits, WMR detected hundreds of lightning discharges, mostly in the polar regions.