AI Re-writeup of the original post by Azaelia in the CE Discord
The Coriolis Effect in the Concave Earth Model
In the Concave Earth model, the Coriolis force exists but arises from distinct mechanisms compared to the conventional convex Earth explanation. The foundation of this phenomenon is rooted in the behavior of a rotating ether wind and the influence of the celestial sphere, which rotates at the center of the concave structure. Here, we explore the nature of the Coriolis effect in the concave Earth paradigm, the forces involved, and how it influences observable phenomena such as wind currents, deflection of objects, and the dynamic equilibrium of the system.
1. The Ether Rotation and the Celestial Sphere
In the concave Earth model, the ether wind plays a fundamental role in producing the Coriolis effect. The ether rotates east to west, driven by the motion of the celestial sphere at the center. This etheric motion causes a form of “resistance” or pressure differential, which interacts with objects, air currents, and other dynamic forces within the concave shell.
The celestial sphere acts as the primary rotating entity that imparts motion to the ether. Rather than being an effect of Earth’s rotation, the Coriolis force in concave Earth is a consequence of the ether wind interacting with the field gradient—sometimes referred to as a bipolar pressure differential.
2. The Nature of the Coriolis Force
The Coriolis effect manifests as deflection of wind, projectiles, or other moving objects due to their interaction with the ether wind. In this model:
- Objects deflect:
- Rightward in the northern regions.
- Leftward in the southern regions.
- This deflection occurs against the grain of the etheric field, which aligns with the celestial rotation.
The etheric pressure spins and lifts away from the Earth’s surface at the equator more than at the poles, creating additional dynamics that influence airflow, cyclonic systems, and the overall movement of matter.
3. Distinguishing the Role of the Coriolis Force
While in the conventional heliocentric model, the Coriolis effect is attributed to the Earth’s spin and centrifugal forces, the concave model redefines these concepts:
3.1. Equatorial Dynamics
In a convex Earth, it is argued that centrifugal force reduces gravitational weight at the equator. However, in the concave Earth:
- The ether wind moves faster at the equator due to proximity to the rotational bulge of the celestial sphere.
- This motion creates less air pressure near the equator because the ether expands slightly due to thermal heating caused by solar energy.
- This lower air pressure, combined with the outward push of the ether wind, reduces the relative weight of objects at the equator.
Key Insight: The bulge at the equator in concave Earth causes a natural push of the ether, which balances the upward deflecting forces at the equator.
3.2. Tangential Velocities
- Objects at the equator exhibit higher tangential velocity in both concave and convex models.
- However, in the concave model, the ether wind’s rotational motion counteracts gravitational inertia. This creates an effect where objects at the equator appear lighter but are still influenced by the celestial sphere’s rotation.
4. Causes of Atmospheric Circulation
The Coriolis effect in the concave Earth is particularly evident in atmospheric movements:
- Air circulates toward the poles as it leaves the doldrums (regions of calm near the equator).
- The ether pressure differential causes the wind to spiral upward and outward toward the celestial sphere’s center at the poles.
This phenomenon creates:
- Cyclones and Hurricanes:
- Vortices are generated due to the rotation of the ether, where cool air from the poles collides with warm air rising from the equator.
- The etheric interaction pushes cyclonic systems into spiral rotations similar to observed behaviors in conventional meteorology.
- Pressure Dynamics:
- The sun’s heat along the tropics reduces air density near the equator, causing air to lift upward. This is enhanced by the centrifugal-like push of the ether, which generates a dynamic low-pressure zone.
5. The Role of the Octahedral Corners
An additional layer of complexity in the concave model involves the octahedral field. The Earth’s concave shell aligns with four tidal equilibrium points at the corners of a central octahedron, which serves as a balancing structure for atmospheric motion.
- The ether equilibrium points create a subtle pressure gradient that adds to the Coriolis effect.
- This results in the north-south equilibrium winds converging at the equator while diverging toward the poles.
6. Observational Consequences of the Coriolis Force
The concave Earth model provides unique explanations for observable phenomena related to the Coriolis effect:
- Wind Deflection:
- Winds move away from the doldrums toward the poles in a spiraling motion.
- Bullets, projectiles, or gyroscopes deflect slightly due to the etheric pressure grain.
- Gyroscopic Rotation:
- A gyroscope, when rotated, exhibits an effect that aligns with the etheric push, resulting in a 15-degree per hour precession.
- Weight Variations:
- Objects weigh slightly less at the equator because the ether bulge generates an upward force, counteracting inertia.
7. Conclusion: The Coriolis Effect in Concave Earth
The Coriolis effect in the concave Earth model is not a result of Earth’s rotation but rather the ether wind influenced by the celestial sphere. The interaction between atmospheric dynamics, etheric pressure gradients, and the sun’s heating creates a system where wind, objects, and forces experience deflections that align with observations attributed to the conventional Coriolis force.
Key mechanisms include:
- The rotating ether moving from east to west.
- The thermal expansion of air at the equator, reducing pressure.
- The bipolar equilibrium of the octahedral structure balancing atmospheric motion.
These principles provide a coherent explanation for the observed atmospheric phenomena within a concave Earth framework, presenting an alternative to the conventional understanding of the Coriolis effect.