We are bounded in a nutshell of Infinite Space: Week 11: Worksheet #20: Problem #1: This is where you live
1.
a.
b. For this
problem, we are attempting to find the range of the distance around a star in
which a planet may have liquid water, what we know as the habitable zone. In
order to understand this, we must find the correlation of temperature and the brightness
of stellar objects. For a planet, we know the Flux it receives from the star it
orbits is: L⋆4πa2=FP,
which can be re written to better represent all the energy impacting
the planet in a specified time: F=Energytime⋅area
L⋆4πa2⋅πR2P=Energytime received by planet
Furthermore,
we should understand the energy the planet then radiates back into space, which
can be described with the equation for bolometric flux: F=σT4P,
and
from previous worksheets we know that the flux can be turned into luminosity by
just multiplying by the surface area LP=σT4P⋅4πR2P
c. Next we
set these equations equal to each other and find the expression for the
temperature of the planet: L⋆4πa2⋅πR2P=Energytime received by planet=LP=σT4P⋅4πR2P
L⋆4πa2⋅πR2P=σT4P⋅4πR2P,
we start simplifying
the equation and find that L⋆4a2=σT4P⋅4π,
which finally turns into: TP=(L⋆16a2πσ)1/4
Also, we
can keep on simplifying the expression were we to consider the definition of
the star’s luminosity: L⋆=4πR2⋆⋅σT4eff,
which can be placed into the equation we just derived to further understand the
factors involved: TP=(4πR2⋆⋅σT4eff16a2πσ)1/4,
TP=(R2⋆T4eff4a2)1/4,
This results in the simplified version of the equation
which expresses the relationship between the planet’s temperature, and the radius
and temperature of the star: TP=Teff√R⋆2a
d. As we
can see from the equations, the radius of the planet becomes insignificant, it
not being a factor in establishing the temperature of the planet, rather the
radius of the star comes into play.
e. Now, we
can assume some energy gets reflected from the surface, yielding an equation
similar to: TP=(L⋆16a2πσ)1/4,
but where A is the energy per time
reflected: TP=(L⋆−A16a2πσ)1/4,
which simplifies to: TP=Teff√R⋆2a−(A16a2πσ)1/4.
Therefore, the temperature most definitely goes
down as the reflectivity increases.
Your expression for (e) is incorrect. The factor A is not an absolute amount of energy but rather a fraction of energy reflected. In other words, A is some number between 0 and 1.
ReplyDeleteThat means that the energy received by the planet from the sun is scaled by a factor of (1-A) which then propagates through the calculation.
The factor A is called "Albedo" if you wanted to look into it further.