Cooling faster in space, or in Antarctica?

In summary: Hmm, I'm not completely sure but my intuition tells me that the function would be:Q = 2pi f(deltaT, r, thermal conductivity of boundary)
  • #1
Blahness
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Here's the situation:

A heated object is in space, with no close proximity to any star. It is simply in one position, motionless.

Another object of equal heat is in Antarctica, in the dead of night, laying half-inside the snow. Temperature at -100 Degrees Celsius.


Which would lose heat faster?
 
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  • #2
Hint: Stefan's Law
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  • #3
But does space have a temperature, since it has so little matter in it?

I'm thinking a vaccum, like how a Thermos works. Is space like a Thermos?
 
  • #4
space is not like a thermos flask. And space does have a temperature, (around 3 Kelvin I think)

Perhaps this makes me a poor experimental physicist, (true) but I've never broken a thermos flask to see how it works. However I think a thermos flask works in two ways, cuts down the heat loss in the body due to convection and conduction via the glass vacuum casing, and reduces heat loss due to radiation via reflection of infrared by the reflective material which the casing employs. Space cuts down on convection and conduction almost completely, I think, but it hardly provides any impediment to radiation loss. So comparing a perfect thermos to a perfect vacuum.. well the thermos is an infinitely better insulator.

As far as the original question goes, (antarctica vs. space), Stefan's law will help you compare radiation heat loss in the two cases, but you would still need to find a way of at least estimating the heat loss in antarctica due to convection and conduction. I can't think how to do this, but I strongly suspect I'd freeze faster in deep space than in antartica deep winter time... heh
 
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  • #5
alfredblase said:
I strongly suspect I'd freeze faster in deep space than in antartica deep winter time... heh
I'd tend to agree, but the answer really depends on how hot this object is and what it's geometry is.

The hotter the object, Blahness, the bigger role radiation plays.
 
  • #6
Blahness said:
Here's the situation:
A heated object is in space, with no close proximity to any star. It is simply in one position, motionless.
Another object of equal heat is in Antarctica, in the dead of night, laying half-inside the snow. Temperature at -100 Degrees Celsius.
Which would lose heat faster?

I think we need some more information.

The object will lose heat due to conduction, convection, and radiation. The radiation law has already been given which will model the heat loss due to radiation. The object half-buried in the snow will only be able to radiate over half the sphere, however.

We now need to know the heat loss of the buried object due to conduction and convection. To compute the heat loss due to conduction we need to know the temperature of the object, the temperature of the snow, and some information about the thermal resistance of the object as calculated from its geometry and conductivity

i.e. heat flow = (thermal conductivity) * (area / length) * (delta-T)

To calculate the heat loss of the buried object due to convection, we need similar information to apply "Newton's law of cooling"

heat flow = (area) * (constant) * (delta-T)
 
  • #7
So the hotter the object is, the more that radiation plays a role in it?

Got it.
 
  • #8
Blahness said:
So the hotter the object is, the more that radiation plays a role in it?

Got it.
I should probably be a little more specific (thorough): The http://www.technifab.com/heat-trans-inter2.htm" shows that heat transfer via radiation increases by a power of four of temperature (T^4, ie, double the temperature difference, and heat transfer increases by a factor of 16), whereas heat transfer via conduction or convection is a simple direct proportion (double the temperature difference and heat transfer doubles).
 
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  • #9
Hmm the question still hasnt been answered properly I don't think. Pervect gave us big clues, without giving any indication as to how his formulas could be applied. The one for conduction he gave I think can only be directly aplied to a case such as two bodies conected by a wire. In the case of a sphere half buried in snow, the "wire" is actually the boundary between the sphere and the snow. Also pervect didnt give the constant needed for the convection formula. In fact determining the constant I think is rather tricky (http://en.wikipedia.org/wiki/Convection) .

Neverheless in the case of conduction the solution can easily be approximated, I think, by a bit of dimensional analysis:

The heat flow at the instant we half bury a sphere in thermal equilibrium in snow is a function of the temperature difference between the sphere and the ice, the thermal conductivity of the boundary and the radius of the sphere. Since we are dealing with only half the surface area buried we can assume it is best to stick a 2pi infront of the function:

Q = 2pi f(deltaT, r, thermal conductivity of boundary)

Now I'm not completely sure but my intuition tells me that the thermal conductivity of the boundary would be the average of the sphere and the snow conductivity as they both contribute equally to the boudary. So Blahness gives us the material and size of the sphere and we can estimate the heat flow due to conduction.

As far as the convection, the problem seems very yucky and unatractive to me, and I'd rather not tackle it for the moment. Maybe later if people continue to show interest in the thread I would give it a bash.

In conclusion and about the radiation dominance:

After considering Russ Watts post, if T_object is of order 10^3 Kelvin or more (and I suspect although I'm not familiar enough with the coductivity and convection constants that that applies if the temperature of order 10^2 Kelvin or more) then there is no contest in that the object will loose heat faster in space. In fact all heat flows due to the three types of loss depend upon area so in comparson, the only factors to worry about are the temperature of the object and the constants of emmisivity, conductivity and convection! Find me those for whichever spherical object you wish and gives us a temperature for it and I will give you a definate answer =) But if you don't want to go to the trouble let's set all the constants to one, after its no big deal hehe, then simply if the temperature of the object is above a certain limit, (if you really want I'll calculate it) then the object in space will loose heat faster! =)
 
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FAQ: Cooling faster in space, or in Antarctica?

How does cooling work in space or in Antarctica?

Cooling in space or in Antarctica relies on the transfer of heat from an object to its surroundings. In space, this is primarily through radiation, while in Antarctica, it is a combination of conduction and convection.

Which cools faster, an object in space or in Antarctica?

An object will cool faster in space because there is no atmosphere to trap heat and slow down the cooling process. In Antarctica, the presence of air and the insulating properties of snow and ice can slow down the cooling process.

Can objects freeze in space?

Yes, objects can freeze in space if they are exposed to extremely low temperatures and there is no source of heat to keep them from freezing. However, most objects in space are designed to withstand these low temperatures and maintain their function even in extreme cold.

How does cooling in space or in Antarctica affect living organisms?

Cooling in space can be harmful to living organisms as their bodies are not designed to withstand the extreme temperatures and lack of heat. In Antarctica, living organisms have adapted to the cold temperatures and have mechanisms to prevent freezing, such as antifreeze proteins in some fish and insects.

Can cooling in space or in Antarctica be used for preservation?

Yes, cooling in space and in Antarctica can be used for preservation as the extreme cold temperatures can slow down or halt biological processes, preventing spoilage and decay. This is why some foods and medications are freeze-dried and stored in Antarctica for long-term preservation.

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