Possible second harmonic gyroemission at Uranus

Astronomy and Astrophysics – Astronomy

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

4

Gyrofrequency, Planetary Magnetospheres, Uranus (Planet), Cold Plasmas, Cyclotron Radiation, Harmonic Analysis, Plasma Density, Ray Tracing

Scientific paper

During the inbound trajectory toward Uranus, the Planetary Radio Astronomy Instrument on board the Voyager 2 spacecraft observed narrow-band smooth (n-smooth) emission at frequencies centered near 60 kHz. By assuming models of the plasma density for the dayside magnetosphere of Uranus and by using cold plasma theory together with stringent observational constraints, ray-tracing calculations were performed to determine the source location and mode of the n-smooth emission. Ray-tracing calculations suggest that the n-smooth emission with sources near the magnetic equator may be fundamental X mode for certain conditions or second harmonic gyroemission. If the emission is second harmonic gyroemission, the fundamental emission at 30 kHz is expected but apparently not observed. These findings are discussed in the context of the most recent developments in the theory of the cyclotron maser instability.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Possible second harmonic gyroemission at Uranus does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Possible second harmonic gyroemission at Uranus, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Possible second harmonic gyroemission at Uranus will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1631710

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.