Calculation of Goldilocks Zone for a given planet and a given star
Calculation of Goldilocks Zone for a given planet and a given star
Distance from a star where water can exist in liquid state (between 273 K and 373 K), calculated with the star’s luminosity and the planet’s albedo
by student Mauro Benjamin Mistretta
Definitions:
Definitions:
Variables:
Planet’s orbit: orbit
temperature on planet’s surface: temperature
star’s luminosity: luminosity
albedo: albedo
Planet’s orbit: orbit
temperature on planet’s surface: temperature
star’s luminosity: luminosity
albedo: albedo
Constants (input in the kernel, within the formulas):
σ = 5.67* W m
AU = 1.4986* m
σ = 5.67*
-8
10
-2
-4
K
AU = 1.4986*
11
10
Planet’s effective temperature (considering albedo)
Planet’s effective temperature (considering albedo)
A planet’s effective temperature is calculated by the means of the formula (1)Where L is the luminosity of the star.The temperature T , for the luminosity and the orbital radius, is:T = ENERGY (the flux) received by the planet’s surface exposed to the star’s light is calculated with the formula:Flux = σ = σ = (2)The planet’s irradiated surface = π where r is the radius of the planet.The total energy received by the planet’s irradiated surface is:E = Flux · Irradiated surface = π = By rearranging the formula (1) , we can calculate the planet’s effective temperature:Effective temperature = = (3)
4
L
4πσ
2
R
4
T
L
4πσ
2
R
L
4π
2
R
2
r
L
4π
2
R
2
r
L
2
r
4
2
R
4
E
4πσ
2
r
4
L
16πσ
2
R
Manipulate[(((((100-albedo)/100)*3.862*10^26*luminosity)/(16π*5.67*10^-8*(1.4986*10^11*orbit)^2))^(1/4)),{luminosity,0.001,100000},{orbit,0.001,200},{albedo,0,100}]
Out[]=
for example: Earth’s albedo 31 , luminosity 1 L⊙ and orbit 1 (AU) yields an effective T = 254.015 K
Orbital radius (in AU) for a planet to have a given effective temperature, albedo and star’s luminosity
Orbital radius (in AU) for a planet to have a given effective temperature, albedo and star’s luminosity
This calculation is achieved by rearranging equation (3):R =
L
16πσ
4
T
Manipulate[((((((100-albedo)/100)*3.862*10^26*luminosity)/(16π*5.67*10^-8*temperature^4)))^(1/2))/(1.4986*10^11),{albedo,0,100},{luminosity,0.1,100000},{temperature,0.1,1000}]
Out[]=
For example, a planet around Tau Ceti (0.5 L⊙ ) should orbit at 0.7 AU in order to receive the same Earth’s solar insolation level (Earth’s effective temperature is 254 K, with an albedo of 31).
Find goldilocks zone with inputs of albedo, star’s luminosity and planet’s surface temperature (boundaries 273 K - 373 K) - output in AU
Find goldilocks zone with inputs of albedo, star’s luminosity and planet’s surface temperature (boundaries 273 K - 373 K) - output in AU
calculation:
calculation:
4
T
flux
noalbedo
4
T
flux
noalbedo
2
r
4
Energyreceived
σ
L
4πσ
4
T
L(insolarluminosities)
4πσ·100/(100-albedo)
4
T
{Manipulate[((((luminosity*3.862*10^26)/(4π*5.67*10^-8*273^4*(100/(100-albedo)))))^(1/2))/(1.4986*10^11),{luminosity,0.00001,100000},{albedo,0,100}],Manipulate[((((luminosity*3.862*10^26)/(4π*5.67*10^-8*373^4*(100/(100-albedo)))))^(1/2))/(1.4986*10^11),{luminosity,0.00001,100000},{albedo,0,100}]}
Out[]=
,
examples (with Earth’s albedo of 31):
Sun : Outer 1.731 AU / Inner 0.927 AU
Vega : 40 L⊙ → Outer 10.951 AU / Inner 5.86625 AU
Proxima Centauri: 0.0017 L⊙ ⟶ Outer 0.07 AU / Inner 0.038 AU
Shaula: 36,300 L⊙ ⟶ Outer 329.89 AU / Inner 176.719 AU
Sun : Outer 1.731 AU / Inner 0.927 AU
Vega : 40 L⊙ → Outer 10.951 AU / Inner 5.86625 AU
Proxima Centauri: 0.0017 L⊙ ⟶ Outer 0.07 AU / Inner 0.038 AU
Shaula: 36,300 L⊙ ⟶ Outer 329.89 AU / Inner 176.719 AU

