Sun's Energy
(spin & fission)

Because we know the spin-energy in both the earth and our sun, along with their surface (atmospheric) temperatures, we can use this information to establish the energy radiated and generated by our sun - including that through fission - by analytic comparison as demonstrated below.

Input Data

The information in this section is known.

Spin Energy

Sun: ES₁ = 1.60097718938751E+35 J (E₂)

Earth: ES₂ = 2.87701820945543E+28 J (E₂)

Orbital Radii & Areas

This Table lists the distances and areas that we can use to establish the stellar radiated heat at our extreme orbital distances; perigee (Rᴾ) and apogee (Rᴬ).

Radius	Value (m)	Area	Value (m²)
Rᴾ	1.47095E+11	Aᴾ	2.71897794748441E+23
Rᴬ	1.52094196155E+11	Aᴬ	2.9069338412793E+23
r₁	6367444.5	A₂	1.27373830409936E+14
r₂	695710000	A₁	6.0822793E+18
Orbital and body dimensions

EME radiated from the sun's surface (Eₛ) is the same at any distance in the universe. However, EME intensity decreases with increasing distance. For example, at earth's perigee and apogee;
Eᴾ = Eₛ . A₂/Aᴾ & Eᴬ = Eₛ . A₂/Aᴬ

Earth's atmosphere (including 2% water vapour)

mass: mᴱ = 5.39513197743931E+18 kg

Energy Capacity: cₚᴱ = 5.30277864707342E+21 J/K

Average Temperatures

There are two heat energy sources in our atmosphere; that supplied by the earth's internal spin-friction and that radiated by our sun.
Given that the mean relative temperature difference is 90K in winter:

perigee = northern hemisphere summer = southern hemisphere winter

apogee = northern hemisphere winter = southern hemisphere summer

Average:    Ṯᴾ = 295 K (perigee)          Ṯᴬ = 280 K (apogee)

Radiated: δṮᴾ = 96.2214665834975 K^# (perigee)          δṮᴬ = 90 K (apogee)

# iterated to ensure Eₛ

Sun's surface temperature: Ṯₛ = 5788 K

Calculations

These calculations define two solar energies based upon the above input data;
a) that radiated from its surface, and;
b) its total internal energy, including spin-friction and fission.

Stored Energy

The seasonal stored energy in the earth's atmosphere is:

perigee: Eᴾ = cₚᴱ.Ṯᴾ = 1.56431970088666E+24 J
apogee: Eᴬ = cₚᴱ.Ṯᴬ = 1.48477802118056E+24 J

Solar EME

The solar radiation proportion of the earth's seasonal atmospheric heat energy, which is based upon δṮ, is calculated thus:

perigee: Eₛᴾ = cₚᴱ.δṮᴾ = 5.10233361421404E+23 J
apogee: Eₛᴬ = cₚᴱ.δṮᴬ = 4.77250078236608E+23 J

because the sun's radiated heat does not vary with earth's orbital distance, its radiation energy should be equal for both seasons:
perigee: Eₛ = Eₛᴾ . Aᴾ/A₂ = 1.0891832323125E+33 J ^#
apogee: Eₛ = Eₛᴬ . Aᴬ/A₂ = 1.0891832323125E+33 J

Solar EME Intensity

The sun's EME intensity at the earth's orbital distance may be calculated thus:
Eᵢᴾ = Eₛᴾ/Aᴾ = 4.00585533737122E+09 J/m²
Eᵢᴬ = Eₛᴬ/Aᴬ = 3.74684561735044E+09 J/m²

Spin:Temperature

Given that our sun's and the earth's matter are similar (albeit in different conditions), their relative spin-friction and radiated EME should also be similar.
Because we know the atmospheric temperature of both celestial bodies, we can compare their relative spin & atmospheric energies using their respective temperatures, the ratios (η) of which should be similar:
cₚ = ES/Ṯ J/K
η = cₚ/ES /K
η = 1/Ṯ /K

Earth:
η₂ = 1/(Ṯᴾ - δṮᴾ) = 0.00503068719187041 /K

Sun:
η₁ = 1/Ṯₛ = 0.000172771250863856 /K

Ratio: η = η₂/η₁ = 0.00503068719187041 ÷ 0.000172771250863856 = 29.1176174665459
The sun's total (internal) energy is 29.12 times as much as that through spin alone. This additional energy is due to the release of fissionable energy in the sun's core.
Fission is the reason bright stars are bright.

Output Data

This section provides the calculation results.

Land & Sea

In our study of the earth's atmosphere we established that 4.00109E+24 Joules of solar EME is absorbed by the earth itself.
This therefore represents an additional solar radiation (energy) as follows:
Eₘ = 4.00109E+24 . ½.(Aᴾ+Aᴬ)/A₂ = 8.8361083773880E+33 J

Solar Radiation

The energy radiated by the sun is therefore;
1.0891832323125E+33 + 8.8361083773880E+33 = 9.9252916097005E+33 J

Total Solar Energy

total: E = ES₁.η = 4.66166413732514E+36 J
fission: EF = E - ES₁ = 4.50156641838639E+36 J

Further Reading

You will find further reading on this subject in reference publications^{(55, 60, 61, 62, 63 & 64)}