solar

SOLAR SYSTEM DYNAMICS

Starlight frees electrons in deep space and solar winds induce a voltage potential between stars and deep space powering solar electric currents which transform voltage potential into kinetic energy until electrical resistance transforms kinetic energy into photons radiated as starlight and radiating the surface of the solar core below the mantle.

At high photon energy, electron positron pair production is the dominant mode of photon interaction with matter. First observed in Patrick Blackett’s cloud chamber, leading to the 1948 Nobel Prize in Physics. If the photon is near an atomic nucleus, the energy of a photon can be converted into an electron–positron pair.

Photons transform into electron positron pairs at the core surface where electrons transform into field lines resulting in residual positrons which merge in trios, three trios are trapped by four transiting electrons and transform into protons which compose the mantle of liquid metallic hydrogen.

The Solid Solar Surface Model is based upon observations from the YOHKOH, SOHO and TRACE satellite programs, from spectral analysis data compiled by the SERTS program. This “running Difference” image of the surface was captured by SOHO. This image was taken on May 27th 2005 at 19:13 using the 195A filter that is sensitive to iron ion emissions.

The mantle is cooled at the surface as liquid hydrogen sublimates into the ionized plasma gas composing the solar wind and interstellar medium which escapes from sunspots and coronal holes. Electrons captured by the solar wind, transform into solar field lines, and transform with protons in endothermic reactions into atoms composing the core surface and exothermic reactions into lighter composing the corona and coronal mass ejected in CMEs.

Temperatures in the corona are upwards of 2 million degrees Fahrenheeit, while just 1,000 miles below, the underlying surface simmers at a balmy 10,000 F. How the Sun manages this feat remains one of the greatest unanswered questions in astrophysics; scientists call it the coronal heating problem.

The planetary fields capture electrons from the solar wind and electrified weather systems charge the planetary surface inducing a voltage potential between the surface and core where electrons transform into field lines and where photons induced by mantle heating transform into protons. The voltage potential powers, core electric currents, which transform with protons into elements

which transform the momentum of moving charges into dipole moments and sum of moments induced by core ions is captured by the solar field which powers super rotation of the solar atmosphere and solar wind, in the direction of core rotation.

The Solar field field is twisted into an arithmetic spiral by the the solar wind traveling anti sunward at a rate of 200–800 km/s, powered by electrical repulsion between solar ions and rotating, powered by moments captured by the solar field making a spiral pattern in space.

A A proto-planetary disk is a rotating disc of ionized gas and dust accreting matter surrounding a young newly formed star, similar to accretion disks around black holes, except accretion discs are hotter and spin much faster.

The three Galilean satellites are involved in orbital resonance, in which the orbital periods of Ganymede, Europa and Io are in a near 1:2:4 ratio and the mutual conjunctions of the Io–Europa pair and of the Europa–Ganymede pair precess around Jupiter at precisely the same rate.

Io and Ganymede are embedded in the high velocity ring current, and block and slow the current which pushes the moons, increasing their velocity, orbital momentum, and radius of their orbits. Io is increasing in mass the fastest of the 3 Galilean moon. One model suggests this resonance was progressively achieved after Io moved outward into a near 2:1 resonance with Europa, and then the Io–Europa pair moved outward until Ganymede was captured into its own near 2:1 resonance with Europa.

The six planets of HD110067 form successive pairs of 3:2, 3:2, 3:2, 4:3, and 4:3 resonances, resulting in the closest planet completing six orbits while the outer-most planet does one.