The solar constant is the same
for the area of the sun's sphere (4πr²) as for the area is its circle (πr²)
Author; Rogelio Perez C
Abstract
The amount of energy that comes from the sun to the
earth is measured with a solar constant. Which has a value of 1364w/m², this
energy is the radiation emission value of the sun for the area of a sphere 4πr², at the
distance of an area of a sphere 4πr² of an astronomical unit, as the earth only receives
sunlight the area of a circle πr², then 4 parts of that energy are not reaching the
earth, so the value of the constant is divided by four, to know how much energy
emitted from the sun enters the earth, but this work shows that the value of
the solar constant does not change when we measure the energy emitted by the
sun, in an area of the solar circle (πr²), between the value of the area of a circle (πr²), of an astronomical unit, which is the area that
looks to the earth, so the division of the solar constant to know how much
energy enters the earth in the area of a circle, should not be divided by 4, as
is currently done.
Introduction;
To know the value of the energy that enters the
planet, we must know the solar constant, but as the part of the energy that
enters the planet is in the area of a circle (πr²), and the solar constant is
the energy value for the area of the sphere (4πr²) of the Sun, then the value
of the solar constant has to be divided into 4 parts, because the value of the
sun's energy in its circle (πr²) is one quarter of that of its sphere. But this
work shows that the energy of the solar constant is the same when we take the
area of the sun sphere, as when we take the area of the sun circle, so the
solar constant should not divide into 4 parts to know the value of the sun's
energy entering the earth at a distance from an astronomical unit.
Theory;
The solar constant, SO, is the total amount of solar
radiation (including all wavelengths of the solar spectrum) per unit of area
that affects in a plane normal to the direction of the solar rays on the
outside of the earth's atmosphere at the average distance between the sun and tierra.1
The average annual solar radiation reaching the upper
part of the Earth's atmosphere (1361W/m²) represents the power per unit of
solar irradiation area through the spherical surface surrounding the sun with a
radius equal to the distance to Earth (1 AU).
This means that the Earth's approximately circular
disk, as seen from the sun, receives approximately stable 1361W/m² at all
times. The area of this circular disk is πr², in which r is the radius of the
Earth. Because the Earth is approximately spherical, it has a total area of
4πr² which means that solar radiation reaching the top of the atmosphere,,
averaged over the entire surface of the Earth, is simply divided by four to
obtain 340 W/m².2
Development;
What is the value of the solar
constant for the area of a sphere 4πr²?
The radiant energy that reaches us from the sun will
decrease inversely to the area formed by a sphere of radius of 1 U.A., that is:
An astronomical unit =1.496E 11M
Astronomical unit in M²=
m²=1.496E 11M x 1.496E 11M= 2,238022E 22m²
Astronomical unit for the radius of a sphere;
=2,23802E+22m²
x 4π 3,14 =2,23802E+22m² x π 12.56=
=2,81095E+23.
Total energy from the sun by the area of a sphere 4πr²;
Formula; E
= σ * A * T⁴
E = sun-radiated heat (Luminosity).
Σ= Stefan-Boltzmann constant.
A =Area of a body (Sun)
T⁴=Temperature raised to 4 power.
Result;
σ = 5,67E-08 W/(M²K4)
A= 6,06679E+18 m²
T⁴= 1,11458E+15 Kelvin4
E = 3,834E+26 Wm²
An area 6.066C10 18m² with a temperature of 5778°k at the fourth power, multiplied by the Stefan-Boltzmann constant, has an energy of 3.834E 26wm²
Then;
The value of the solar constant= to the energy emitted
by the sun in the area 4πr² of a sphere= 3.834E 26w/m², between the astronomical unit in
the area of a sphere 4πr²=2, 81095E+23m²
3.834E 26w/m² /2, 81095E+23 = 1363.953709w
The value of the solar constant is equal to 1364wm²
What is the solar constant value
for the area of a circular disc πr²?
An astronomical unit =1.496E 11M
Astronomical unit in M²=
m²=1.496E 11M x 1.496E 11M= 2,238022E 22m²
Astronomical unit for the radius of a circle πr²;
=2,238022E 22m² x π 3.14 = 7,027E 22m²
Energy emitted by the sun for the
area of a circle πr².
Formula; E
= σ * A * T⁴
E = sun-radiated heat (Luminosity).
Σ= Stefan-Boltzmann constant.
A =Area of a body (Sun)
T⁴=Temperature raised to 4 power.
Result;
σ = 5,67E-08 W/(M²K4)
A= 1,5167E+18m², m²
T⁴= 1,11458E+15 Kelvin4
E = 9,58501E+25 wm²,
An area 1,5167E+18m², with a temperature of 5778°k
at the fourth power, multiplied by the Stefan-Boltzmann constant, has an
energy of 9,58501E+25 wm²,
Then;
The value of the solar constant= to the energy emitted
by the sun in the area of a circle (πr²).= 9,58501E+25 wm², between the astronomical unit in
the area of a circle (πr²).= 7,027E 22m²
9,58501E+25 wm²/ 7,027E 22m² =
1363.953709w
Value of the solar constant for the circle (πr²). of the sun is
equal to 1364wm²
Conclusion;
The solar constant for the Earth is equal to the
energy emitted by the sun for a radius of a sphere, than for the radius of a
circle, so the temperature that reaches us from the sun to the top of the
atmosphere, should not be divided by 4, since the Solar constant does not
change the energy value.
Bibliography;
1- file:///C:/Users/MASTER/Desktop/radiacion.pdf
2-https://en.wikipedia.org/wiki/Solar_irradiance

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