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 only in General terms describes the mechanism of tides, 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 behavior 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 the 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 a certain resistance to its movement along the surface of the Earth because of water’s own viscosity and friction by the bottom and the shore. To paraphrase all of the above: the movement of water reflects the speed of the ether with some rough approximation.
The velocity of solids 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 presence 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 in general the mechanism of transmission of motion from ether to water, we can proceed to the analysis of fluctuations in the ether. The real ethereal flow that the 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, created 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-ether” interaction that takes place before the ether contacts the substance.
Daily tides are created 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.
The lunar tides
The same mechanisms apply in the case of lunar half-day and daily tides, only in this case the duration of half a day is 12 hours, 25 minutes.
The fact that the Moon does not rotate around its own axis does not change the behavior of the ether that the Moon absorbs. This ether revolves around the Moon in the same way as it revolves around other celestial bodies with gravity.
The lunar ether vortex is not strong enough to overcome the tidal influence of the Earth, and to spin the moon (the so-called tidal lock – see the half-day solar tidal mechanism – which acts in the direction of braking the axial rotation of the Earth).
Super-rotation of atmosphere
It is worth mentioning here that the discussed above tidal block mechanism is also related to the super-rotation of the atmosphere, which is observed when a celestial body is a satellite having its own gravity and atmosphere, has an orbit too close to the host planet or star. As is the cases with Venus or Titan, which are both close enough to their central gravitational partners to become tidal-blocked satellites, and both have atmospheres that make the super-rotation effect visible. The effect of super-rotation allows us to see the rotation of the gravitational vortex of the ether due to the atmosphere having more freedom to follow the rotating ether than the celestial body itself, which producing the ether vortex.
Back to the Moon’s half-day tides.
In the figure below, solar gravity has the same effect on the Earth and on the Moon, so we do not take solar gravity into account at this stage of our analysis. Also, the rotation of the ether caused by the Earth’s gravity is synchronized with the daily rotation of the Earth, so we do not take into account the Earth’s gravity. This approach in the analysis of the half-day tides caused by the Moon leaves us to consider only the lunar gravity.
Also, this approach along the way (gives an answer to) reveals a very important fact to which orthodox explanations of tides give a completely unsatisfactory answer. The question is, “Why does the Moon, which has very little gravity on the Earth’s surface compared to Solar gravity, have a much stronger tidal effect on the Earth?»
The answer given by the Law of Mechanics: the Earth is at rest relative to the combined solar-terrestrial gravitational vortex. But the Lunar vortex, despite its relative weakness, is not compensated at all, and is entirely applied to the Earth. The lunar gravitational vortex constantly changes its position relative to the Earth.
In fact, tides are caused by the Earth’s own rotation as such, or more precisely – tides are caused by the interaction of the Earth with the surrounding ether, we mentioned this earlier, speaking about the principle of locality. The Moon and the Sun only affect the shape and behavior of the ether that surrounds them; there is no direct interaction between the Earth and the Sun or the Moon.
This also explains why there are time delays between the highest or lowest tides and the extremes in the Moon’s position (the so-called tide age). The Earth always interacts with the ether, which is in direct contact with the Earth; and the ether, which was under the influence of the Moon, takes time to convey its state to the ether in contact with the Earth. Therefore, the Earth’s gravitational vortex reaches the corresponding state of the highest or lowest tide somewhere further in space; and the corresponding position depends on the trajectories and characteristics of all participants in the interaction: the Sun, Moon, Earth and Ether. Therefore, it is so difficult to recognize a certain pattern responsible for apparently unpredictable tidal delays.
Knowing these delays gives us valuable information about the properties of the ether — such as its speed and ability to maintain shape and movement.
Lunar diurnal tides
As we can see from the illustration for the lunar daily tides, its mechanism uses the same principle as the solar daily tides.
The main difference between the Solar and Lunar daily components of tides:
— In the case of the Moon – the effect of weak lunar gravity at a distance of 300,000 kilometers affects the Earth’s gravity.
— In the case of the Sun – the stronger gravity of the Earth at a distance of 0 km, affects the solar gravity.
Therefore, the lunar daily tides are the smallest components of the four main tidal components. In addition, the lunar diurnal mechanism produces the least inhibitory effect on the lunar semi-diurnal component, thus helping the lunar semi-diurnal component to be the largest of the four major tidal components.
There is also a strong dependence of the lunar daily tides from the declination of the moon, and the greater the declination (the deviation of the moon’s orbit from the equator) in one direction or another, the greater the amplitude of the daily tides. This can also be explained by our theory, since the daily tides are not the effect of direct action, but influence the half-day tides, modifying them, also here asymmetric modulation plays its role. The greater the modulation asymmetry, the more noticeable it is.
The full description of the tides is not so simple. It should include a large number of other effects and factors that determine the behavior of tides at a certain place at a certain time. Some of these factors, especially the tilt of the earth’s axis and the parameters of the lunar orbit, may be worth considering in a separate article later. But now, our goal is to show in general terms:
a) a mechanism that directly creates tidal currents — as an alternative to the universally accepted belief in “tidal humps” rolling around the Earth, and being the root cause of tidal currents;
b) two periodic forces that create two independent, simultaneous waves, one with a daily, and one with a half-day period. Instead of the generally accepted belief in the existence of a single mechanism of tides with a half-day frequency; and the formation of the daily component as a subharmonic of a half-day component.
(c) Please do not confuse this paragraph with paragraph ”a”, which deals with the direct mechanism of the tidal forces. Here we are talking about the celestial bodies causing gravitational flows of ether, which then after a certain period of time come into contact with the Earth, and begin to act on it.
The Sun and the Moon are act upon Earth by their gravity not directly, but indirectly, through the ether. This creates delays and shifts in the application of tidal forces.
This in particular explains the efficiency of the method of so-called “fictitious luminaries”, which is used by official science. Indeed, tides are not caused by the Sun and the Moon directly by the direct action of the “gravitational force” (no matter what speed of action). In fact, the tides are caused indirectly by the Sun and the Moon disturbing the ether around them. And only then, the Earth comes into direct contact with the traces of the impact on the ether left by celestial bodies in the form of an agitated ether. In this case, there is the illusion of the action of fictitious luminaries, since the position of the moon does not coincide with its delayed effect.
At this point, we will finish the analysis of tides, as at the moment other topics related to rotational gravity, are much more important for understanding the world around us based on the Law of Mechanics. Such topics are stellar aberration and parallax, which are discussed in the next section.
The theme of tides is interesting mainly as an example of the application of the Law of Mechanics to the problem, which was not resolved by the official science. It would be unproductive to spend too much time on the tides now, it is enough to consider this topic in general and move on.
The Law of Mechanics 