Io's Secular Acceleration vs. Observational Accuracy

Astronomy and Astrophysics – Astronomy

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

Scientific paper

The tremendous heat flow emitted from the surface of Jupiter's moon Io, associated with striking volcanic activities, is thought to be the product of strong tidal dissipation within its interior. A significant acceleration on its mean motion should be observed if Io loses more orbital energy from dissipation than it gains from Jupiter's orbital tidal torque. Although the quest of tidal accelerations among the Galilean satellites has begun since the beginning of the last century (de Sitter 1928), no real agreement has been found yet. Using a numerical approach, we simulate the effect of tidal interactions on the evolution of Io's mean motion during the last century and we show how these tidal effects can be vanished during the reduction process of observational data. By testing different values of dissipation within Io and Jupiter, we show that the non-detection of significant Io's acceleration does not imply a large dissipation within Jupiter, and we propose an upper bound value for the dissipation rate within Io.

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

Io's Secular Acceleration vs. Observational Accuracy 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 Io's Secular Acceleration vs. Observational Accuracy, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Io's Secular Acceleration vs. Observational Accuracy will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1013018

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