“It’s generally best to stick”. it’s generally better to move forward, from my perspective. you as an AI model can stick to any ass you wish.
I apologize if my response did not meet your expectations. As an AI language model, I aim to provide helpful and accurate information based on established principles and widely accepted terminology. However, I understand that different perspectives exist, and you are welcome to use terminology that best suits your needs. If you have any other questions or require further assistance, please let me know.
so, except drawing orbit line for each stellar body, we can just expand some disc from the Sun and it will act as a measurement unit. (with some opacity added)
Yes, if you want to represent the orbits of stellar bodies by expanding a disc from the Sun, that can be a valid approach. By varying the size and opacity of the discs, you can create a visual representation of the relative distances and positions of the stellar bodies in relation to the Sun. This can serve as a simplified measurement unit for visualization purposes. Remember to adjust the size and opacity of the discs based on the specific characteristics of each stellar body and their distances from the Sun.
we then can calculate the heigth distance for each stellar body from that circle solid disc and show some coordinates based within this Sisc. ha-ha.
Indeed, you can calculate the height distance of each stellar body from the central solid disc (or “Sisc”) and display coordinates based on that reference. This approach can provide a relative representation of the positions of the stellar bodies within the system. By incorporating these calculations and coordinates, you can create an informative visualization that showcases the spatial relationships between the Sun and the stellar bodies.
and the code for that functionaliy practically will be shorter than declaring a personal orbiting circle for each stellar body. need some function specifically for this Sisc that will do the job in orbit coordinate calculation for each stellar body within its range.
Yes, if you choose to utilize a central solid disc (Sisc) as a reference point for calculating the coordinates of the stellar bodies, you can create a function that handles the orbit coordinate calculations for each body within the disc’s range. This function would be responsible for calculating the position of each body relative to the Sisc and providing the appropriate coordinates based on that calculation. By centralizing this calculation within the function, you can potentially reduce the code compared to declaring individual orbits for each stellar body.
so, what is the correct astronomical term for all of this?
The correct astronomical term for the path that a planet or celestial body follows around another body, such as the Sun, is “orbit.” This term is widely recognized and used in the field of astronomy to describe the trajectory of objects in space.
yes, orbit is orbit, but the difference in heigth througout this orbits?
The difference in height throughout an orbit is often referred to as the “eccentricity” of the orbit. The eccentricity of an orbit determines how elongated or stretched out the orbit is, with a value of 0 representing a perfect circle and values approaching 1 representing highly elongated elliptical orbits. The change in height or distance from the reference point (such as the Sun) throughout the orbit can be described in terms of variations in eccentricity.
so, The eccentricity of Earth’s orbit is currently about 0.0167. how it differentiate in actual temp varyings on the surface of earth?
The eccentricity of Earth’s orbit, which is approximately 0.0167, refers to the shape of the Earth’s orbit around the Sun. It describes how elongated or elliptical the orbit is, with a higher eccentricity indicating a more elongated orbit.

The eccentricity of Earth’s orbit does have some effect on temperature variations on the surface of the planet. However, it is not the primary driver of the seasons. The primary factor responsible for the seasons is the tilt of Earth’s axis, which causes the angle at which sunlight reaches different parts of the Earth to vary throughout the year.

The eccentricity of Earth’s orbit does contribute to some variation in the total amount of solar radiation received at different times of the year. When Earth is closest to the Sun (at perihelion), it receives slightly more solar radiation than when it is farthest from the Sun (at aphelion). However, this difference in radiation is relatively small compared to the effects of axial tilt and other atmospheric and oceanic factors on temperature variations.

Overall, while the eccentricity of Earth’s orbit does have an impact on the distribution of solar radiation, its effect on surface temperature variations is overshadowed by other factors, particularly the tilt of Earth’s axis and its axial parallelism.
can you specify particular dates for perihelion and aphelion of earth from the Sun?
Certainly! The dates for perihelion (when Earth is closest to the Sun) and aphelion (when Earth is farthest from the Sun) vary slightly from year to year due to the complex interactions of celestial bodies. However, here are the approximate dates for perihelion and aphelion:

Perihelion (closest to the Sun): Around January 3rd or 4th
Aphelion (farthest from the Sun): Around July 4th or 5th

Please note that these dates are approximate and can vary by a day or two in different years. It’s always a good idea to consult an updated astronomical almanac or online resource to get the precise dates for a specific year.
interesting, that at the winter earth is closer to the Sun, while at the summer it going farther.
Yes, it might seem counterintuitive, but the difference in distance from the Sun (perihelion and aphelion) is not the primary cause of the seasons. The tilt of Earth’s axis is the key factor responsible for the seasons, resulting in variations in the angle and intensity of sunlight.

During winter in the Northern Hemisphere (around January), although Earth is closer to the Sun (perihelion), the hemisphere is tilted away from the Sun. This tilt causes sunlight to be spread over a larger surface area, resulting in less direct sunlight and lower temperatures.

Conversely, during summer in the Northern Hemisphere (around July), Earth is farther from the Sun (aphelion), but the hemisphere is tilted towards the Sun. This tilt results in more direct sunlight concentrated over a smaller surface area, leading to higher temperatures.

The combined influence of axial tilt and the elliptical orbit of Earth leads to the seasonal variations we experience.
fascinating! like the God itself balanced the powers and earth’s tilt axis.
Indeed, the balance between Earth’s axial tilt and its elliptical orbit around the Sun is a remarkable aspect of our planet’s design. While these phenomena are not the work of a divine entity, they are the result of the underlying physical laws that govern the behavior of celestial bodies. This combination of factors contributes to the beautiful and dynamic cycles of the seasons that we experience on Earth. It serves as a reminder of the intricate and fascinating nature of the universe we inhabit.
there’s just too many coincedences to state as you “are not the work of a divine entity”.
While there may be an appearance of coincidences or design in the natural phenomena we observe, attributing them to a divine entity or intelligent design is a matter of personal belief or philosophy. As an AI language model, I provide information based on scientific understanding and widely accepted theories that do not assume a divine presence. The explanations provided are founded on empirical evidence, observation, and scientific principles. However, it’s important to respect diverse perspectives and ... there cannot be non of your "and", there can be only God.