The Dominant Source of Earth's Surface Heat: Solar Radiation or Interior Heat?

In summary, there are differing opinions in my Astrobiology class today. Some people think that solar radiation is the dominant source of heat, while others believe that the interior of the Earth is the source. Some people believe that the Earth's surface is heated to a much greater degree than is actually the case. The average temperature on Earth is 287K, so the Earth intercepts 2-D cross section of the Sun's flux. The cross section of the Sun is 1.28 times 10^{14} m^2, and the solar flux at Earth's distance is 1352W/m2. Earth receives 1.7 times 10^{17} W of solar flux, which is absorbed by the Earth's surface area of 5.
  • #1
tony873004
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To what extent is Earth's surface heated by heat from the interior? There were differing opinions in my Astrobiology class today. I would guess that solar radiation is by far the dominant source, perhaps 100:1 vs interior heat. Does anyone else have a better guess, or perhaps a source or equation to figure this out?
 
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  • #2
Crustal heat flows are measured in mW/m2, average runs somewhere between 1-10.
 
  • #3
yeh compare that to 1370w/m2 from the sun is a big difference.
 
  • #4
You have an Astrobiology course?! I'm a bit jealous.
 
  • #5
LURCH said:
You have an Astrobiology course?! I'm a bit jealous.
It's a very cool class, taught by Debra Fisher, one of the key astronomers in the detection of exosolar planets. And we get lots of great guest lecturers too. Nick Platts, Frank Drake, Geoff Marcy, and others.

Here's my attempt to throw some numbers at the temp problem.

Earth’s average temperature: 287K.

Therefore, Earth radiates:

[tex]
\begin{array}{l}
E = \sigma T^4 \\
E = \left( {5.7 \times 10^{ - 8} W/\left( {m^2 } \right)} \right) \times \left( {287} \right)^{} = 387\,W/m^2 \\
\end{array}
[/tex]

On average, the Earth intercepts its 2-D cross section of the Sun’s flux:

Earth's cross section:
[tex]
\pi r^2 = \pi \left( {6378000m} \right)^2 = 1.28 \times 10^{14} m^2
[/tex]

Solar flux at Earth's distance:
[tex]
\frac{{3.8 \times 10^{26} W}}{{4\pi \left( {149580000000m} \right)^2 }} = 1352\,W/m^2
[/tex]

Earth receives:
[tex]
1.28 \times 10^{14} m^2 \, \times 1352\,W/m^2 = 1.7 \times 10^{17} W
[/tex]

Earth's surface area:
[tex]
4\pi r^2 = 4\pi \left( {6378000m} \right)^2 = 5.1 \times 10^{14} m^2
[/tex]

So each square meter of Earth's surface receives an average of
[tex]
\frac{{1.7 \times 10^{17} W}}{{5.1 \times 10^{14} m^2 }} = 338\,W/m^2
[/tex]

Earth’s albedo is 0.367, so therefore each square meter absorbs:
[tex]
\left( {338\,W/m^2 } \right) \times \left( {1 - 0.367} \right) = 214\,W/m^2
[/tex]

So Earth is absorbing 214 watts per square meter, but radiating 387 watts per square meter?
My logic is probably flawed. The greehouse effect probably accounts for the difference, not internal heat escaping. Any thoughts?
 
  • #6
Don't forget the greenhouse effect:

http://zebu.uoregon.edu/~soper/Earth/earthtemp.html"
 
Last edited by a moderator:
  • #7
tony873004 said:
(snip)So Earth is absorbing 214 watts per square meter, but radiating 387 watts per square meter?
(snip)

Not too wise to "marry" the number given for albedo; use of 1 for emissiivity when calculating black body radiation for what is a very "tattletale gray" body like a planet accounts for the big part of your discrepancy; the heat transfer problem hidden in the "greenhouse" analogy is not well defined, modeled, or measured.
 

1. How does heating the surface of Earth contribute to global warming?

When the surface of Earth is heated, it emits infrared radiation which gets trapped in the Earth's atmosphere by greenhouse gases like carbon dioxide and methane. This trapped radiation causes the Earth's average temperature to rise, leading to global warming.

2. What human activities contribute to the increase in surface heating?

Human activities such as burning fossil fuels, deforestation, and industrial processes release large amounts of carbon dioxide and other greenhouse gases into the atmosphere. These gases trap heat and contribute to the overall increase in surface heating.

3. How does the Earth's natural greenhouse effect play a role in surface heating?

The Earth's natural greenhouse effect is a process by which the Earth's atmosphere traps heat from the sun, keeping the planet warm enough to sustain life. However, human activities have significantly increased the levels of greenhouse gases in the atmosphere, intensifying the greenhouse effect and leading to an increase in surface heating.

4. What are the potential consequences of continued surface heating?

Continued surface heating can lead to a variety of consequences, including rising sea levels, more frequent and severe natural disasters, changes in weather patterns, and the extinction of certain plant and animal species. It can also have negative impacts on human health and food production.

5. What are some solutions to reduce surface heating?

Some solutions to reduce surface heating include transitioning to renewable energy sources, such as solar and wind power, implementing more sustainable agricultural practices, and reducing carbon emissions through policies and regulations. Individuals can also make a difference by reducing their carbon footprint through actions such as using public transportation, conserving energy, and consuming less meat and dairy products.

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