Приклади вживання Orbital resonance Англійська мовою та їх переклад на Українською
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Ganymede is in a three-way orbital resonance with Io and Europa.
In current theories,planet migration facilitates objects coming into orbital resonances.
Currently Ariel is not involved in any orbital resonance with other Uranian satellites.
He moves in orbital resonance with the Earth and, in theory, would crash into it in a few million years.
Currently Umbriel is not involved in any orbital resonance with other Uranian satellites.
Orbital resonances greatly enhance the mutual gravitational influence of the bodies, i.e., their ability to alter or constrain each other's orbits.
The moons may have been caught in and then escaped from orbital resonance several times;
This outward migration involved orbital resonances between Jupiter and Saturn, and between Saturn, Uranus, and Neptune.
A large number of Kuiper belt objects, like Pluto, are in a 2:3 orbital resonance with Neptune.
Ganymede participates in orbital resonances with Europa and Io: for every orbit of Ganymede, Europa orbits twice and Io orbits four times.
The dashed lines indicate the Kirkwood gaps, where orbital resonances with Jupiter destabilize orbits.
At the time of discovery, Gliese 876 was known to host two extrasolar planets,designated Gliese 876 b and c, in a 2:1 orbital resonance.
For instance, we know that Neptune and Pluto are in orbital resonance- for every two orbits Pluto makes around the sun, Neptune makes three.
MS4 belongs to the class of dynamically hot Kuiper belt objects.[15]It is in an intermittent 18:11 orbital resonance with Neptune.
Orbital resonance- Orbital resonances greatly enhance the mutual gravitational influence of the bodies, i. e. their ability to alter or constrain each others orbits.
Ganymede orbits Jupiter in roughly seven days and is in a 1:2:4 orbital resonance with the moons Europa and Io.
It was thought there could have been multiple orbital resonances at work between Charon and the small satellites that would move the small satellites into their current orbits.
Completing an orbit in roughly seven days,Ganymede participates in a 1:2:4 orbital resonance with the moons Europa and Io.
The subsurface ocean may have resulted from a 2:3 orbital resonance between Dione and Tethys early in the Solar System's history that led to orbital eccentricity and tidal heating of Tethys's interior.
Completing an orbit in roughly 7(seven) Earth days,Ganymede participates in a 1:2:4 Orbital Resonance with the other Jovian moons Europa and Io.
Since each orbital resonance provides a geometric relationship between the bodies involved, the resonant configurations of these KBOs can help point astronomers to the right spot in our Solar System to find it.
Using this same reasoning, they hypothesized that the KBOs examined by Batygin andBrown might be in an orbital resonance with the Planet 9.
They may have been caught in and then escaped from orbital resonance several times; they currently are in or at least close to an 8:3 resonance. .
The first hints of a subsurface ocean came from theoretical considerations of tidal heating(aconsequence of Europa's slightly eccentric orbit and orbital resonance with the other Galilean moons).
A past 3:1 orbital resonance between Miranda and Umbriel and a past 4:1 resonance between Ariel and Titania are thought to be responsible for the heating that caused substantial endogenic activity on Miranda and Ariel.
A Lindblad resonance, named for the Swedish galactic astronomer Bertil Lindblad,[1]is an orbital resonance in which an object's epicyclic frequency(the rate at which one periapse follows another) is a simple multiple of some forcing frequency.
The physics principle behind orbital resonance is similar in concept to pushing a child on a swing, where the orbit and the swing both have a natural frequency, and the other body doing the“pushing” will act in periodic repetition to have a cumulative effect on the motion.