How hot does Gaseous H2O need to be to emit IR Photons?

AI Thread Summary
Gaseous H2O emits infrared (IR) photons primarily in the ten-micron range, with conditions for emission influenced by temperature and pressure. The temperature required for significant photon emission correlates with black body radiation principles, where peak frequency is temperature-dependent. Water vapor is not an ideal blackbody, leading to limited IR radiation compared to a perfect blackbody. The ten-micron band is crucial for understanding atmospheric phenomena, as it contributes to the IR "windows" in humid conditions and affects nighttime temperatures by producing "back" radiation. Overall, the interaction of water vapor with IR radiation plays a significant role in meteorological observations and climate dynamics.
Michael Thornton
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I've read that H2O has an absorption/emission band around to 10 micron range. What conditions are required for photons of this wavelength to be emitted by H20 gas? In particular, how hot would the gas have to be? What amount of pressure is required? Under everyday conditions (like steam possible to detect an appreciable amount of these photons?

Also, how would you determine this for any wavelength absorption/emission band?

Thanks for any and all responses!
 
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"Ten microns?" Room T.
 
Bystander said:
"Ten microns?" Room T.

Ten micrometers
 
Bystander knows what a micrometer is: he was answering your (main) question. To answer the follow-up question, it is a function of black body radiation (equations on its wiki page), with the peak frequency corresponding to the temperature:
BlackbodySpectrum_loglog_150dpi_en.png
 
Ok, I guess I'll need to be more specific.

How much IR light would be radiated compared to a blackbody? I'm under the impression that water vapor is not a very good blackbody, so I'm trying to understand that idea a little better.
 
I don't have specific answers, but I'd look into this in the context of weather forcasting: ir satellite photos of water vapor is one of our better tools for it.
 
Actually, water vapor is fairly transparent to the ten micron wavelength band. That is why that band forms one of the humid atmosphere's IR "windows". On the other hand, liquid water absorbs it quite nicely. This band is one of the major sources of terrestrial IR for clouds, and the reason cloudy nighttime skies are "warmer" than clear ones. They produce "back" radiation to the Earth's surface that is absent under clear skies. This radiation, in turn, comes in large part from the warming caused by the absorption of the ten micron band. This band is the peak wavelength in the surface IR emissivity.
 
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