and other effects caused by the rotational component of gravity
One of the most obvious effects of rotational gravity is the phenomenon of tides, but at the same time, this phenomenon is quite difficult to analyze. Therefore, this section describes the mechanism of tides only in general terms, avoiding details. Needless to say, our explanation of tides is completely different from the orthodox explanation.
First of all, let’s define the general principles of our approach.
First: water, like any liquid, is a material body that has freedom of movement with ether. That is, if the ether is accelerated, the water is accelerated along with the ether. This behaviour is typical for bodies that are not restricted in their movement by other bodies.
The situation when bodies have complete freedom of movement with ether (weightlessness) was considered in the first Chapter of this work — introduction to the Law of Mechanics. But in the case of tides, we can only talk about relative freedom of movement of water with ether — only along the surface of the Earth. The movement down, following the absorbed ether, is prevented by the Earth’s surface.
The relativity of the freedom of movement of water is also in the fact that the water meets certain resistance to its movement along the surface of the Earth because of water’s own viscosity and friction by the bottom and the shores. To paraphrase all of the above: the movement of water reflects the speed of the ether with some rough approximation.
The velocity of solid bodies stationary on the Earth is equal to the velocity of the Earth’s surface, and these solids only “feel” the forces of inertia applied to them from the ether, but do not shift when the ether accelerates through them. Unlike solids, water changes its speed along with the speed of the ether, and “feels” the forces of inertia only in case of meeting any solid obstacles in its path.
Thus, in our analysis of tides based on the Law of Mechanics, we will review changes in the speed of the ether relative to the Earth’s surface at different orientations relative to the Sun and Moon. The acceleration of the ether in this case plays a secondary role.
The second principle point is related to the nature of the interaction of celestial bodies, in this case the Earth, the Moon and the Sun. Tidal interaction is conveyed through the ether. The Earth interacts only with the surrounding (local) ether, the Sun and the Moon also interact only with the surrounding (local) ether. This can be called the principle of locality, more about this principle in the section devoted to space and time. In the case of tides, this principle is very clear and macroscopic, making it very understandable.
In this Chapter, we will try to explain the reality of the existence of two individual (independent) tidal mechanisms: daily and semi-daily, and examine the processes that cause them.
Solar semi-diurnal component of the tides
This component of the tides, considered individually, is a mechanism that directly transmits the movement of the ether to the water. Reviewing separately the solar half-day component, we suppose that the ether surrounding the Earth moves only under the action of the Sun without any other disturbances. And the planet Earth just moves along with this ether and rotates in this uniform flow without exciting any of its own ether vortexes. Such simplification allows to extract the final phase of originating of tides, — a phase of interaction of a near-earth ether with water.
The first case is a half-day (twice a day) component of the tides.
The picture below shows in the most general terms the interaction of two celestial bodies, blue – Earth, and red – Sun.
Half-day tides occur because the earth’s axial rotation creates a difference in relative velocity between the Earth’s surface and the surrounding ether. For each given location, this speed difference increases and decreases twice a day, and all the time it has the same direction.
When a given surface of the Earth faces the Sun, the velocity of the Earth’s axial rotation is subtracted from the Earth’s orbital velocity, making the resulting velocity of that surface less than the velocity of the surrounding ether, which moves at the Earth’s orbital velocity. This surface will experience the force exerted by the ether accelerating through the earth’s surface (according to the Law of Mechanics). This tidal force will create stresses inside the solid Earth, and the flow of water in the ocean directed against the direction of rotation of the Earth (from East to West). And for the same reason, when the same surface is facing in the direction opposite to the Sun, the speed of the earth’s axial rotation is added to the Earth’s orbital speed, making the speed of this section of the surface faster than the speed of the surrounding ether. This will create a tidal flow in the same direction – from East to West. As a result – twice a day we have a tidal current in the same direction, and twice a day no current.
We started with the solar half-day component because the solar etheric vortex is dominant. Gravitational vortices produced by all other celestial bodies are only superimposed on the solar vortex, modifying its direction and speed.
After reaching understanding of the mechanism of transmission of motion from ether to water in general, we can proceed to the analysis of fluctuations in the ether. The real ethereal flow that Earth encounters is not uniform and homogeneous. It is constantly distorted by the gravity of the Earth itself, the Moon and other celestial bodies. These distortions are responsible for the presence of various components of the tides. Most of these influences have a periodic nature and can be estimated, it is only necessary that these computations had a conscious nature, that is, made in accordance with a clearly comprehended physical mechanism.
Solar diurnal component of tides
The second case – daily (once a day) components of tides.
The picture below illustrates the daily tidal mechanism. This is the “ether-to-ether” interaction that takes place before the ether contacts the substance.
Daily tides are produced because of the interaction of the rotating flow of ether (a vortex created by the Earth’s own gravity) with the orbital flow of ether, which moves the Earth around the Sun. In other words, the daily tides are the result of the modulation of the orbital stream of the ether by the gravitational vortex of the Earth.
On the Sun-facing side of the Earth, the ether, which rotates synchronously with the Earth, slows the ether moving in the opposite direction (30 km/s – 0.465 km/s). This creates a slowdown in the resulting flow of ether interacting with the Earth’s surface, and as a result – the flow of water in the direction from East to West.
When the same surface looks in the opposite direction from the Sun, the ether rotating with the Earth accelerates the orbital flux of the ether caused by the Sun and moving in the same direction (30 km/s + 0.465 km/s). This creates an acceleration of the resulting flow of ether, and as a result – the flow of water in the direction from West to East.
As we can see, this mechanism also causes two water flows and two stops, but the directions of the two flows are opposite, so during the day we have one tide and one ebb.
As we can see, the second (daily) tide mechanism works in the direction of reducing the effect of the first (half-day) tide mechanism. This compensation is not complete; it only reduces the resulting force of the solar half-day tides. Therefore, the half-day component of the solar tides is less than the daily component.