Difference between revisions of "Optical Depth"

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A useful real world example of optical depth is fog. Within a fog cloud (see image above), nearby objects are clearly visible and distant objects are completely obscured. At intermediate distances, objects are difficult but not impossible to discern. In the image above, the tree to the left corresponds to an optical depth of approximately 1, since it is mostly obscured, though still visible. The person in the foreground is at an optical depth of less than 1 (perhaps around 0.5), since they are easily discernable and there is very little fog blocking light between the person and the observer. Lastly, the end of the road is at an optical depth much greater than 1, since it is completely covered over by the fog and invisible to the observer.
 
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A useful real world example of optical depth is fog. Within a fog cloud (see image above), nearby objects are clearly visible and distant objects are completely obscured. At intermediate distances, objects are difficult but not impossible to discern. In the image above, the tree to the left corresponds to an optical depth of approximately 1, since it is mostly obscured, though still visible. The person in the foreground is at an optical depth of less than 1 (perhaps around 0.5), since they are easily discernable and there is very little fog blocking light between the person and the observer. Lastly, the end of the road is at an optical depth much greater than 1, since it is completely covered over by the fog and invisible to the observer.
 
  
 
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Revision as of 18:10, 11 December 2018

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Optical Depth

Solving for specific intensity in the Radiative Transport Equation

for zero emission () gives a solution of the form:

where is the optical depth at . Optical depth is often computed as:

where , the column density, is in and is the # of extinguishers per unit area. Similarly,

where is the mass surface density.

The Mean Free Path is given by: . Thus:

That is, the optical depth is the number of mean-free-paths deep a medium is. For Poisson processes, the probability of absorption is given by:

Therefore:

In fact, the radiative transport equation can be expressed in terms of optical depth. Dividing by and recognizing :

where is a “source function”. In general,

There is a formal solution for . Let’s define and . Then:

If is constant with , then:

That second term on the righthand side can be approximated as for , since self-absorption is negligible. Similarly, for , it may be approximated as . The source function is everything. It has both the absorption and emission coefficients embedded in it.

Examples

Mona lisa vs radius.png
An example of the Mona Lisa at optical depth of , for obscuring particles of various radii. To achieve the same optical depth, particles with a smaller cross-sectional area need to have a higher column density.
Mona lisa vs opt depth.png
The Mona Lisa at various optical depths, illustrating how the transition from optically thin to optically thick erases the background picture.
Fog.png
A useful real world example of optical depth is fog. Within a fog cloud (see image above), nearby objects are clearly visible and distant objects are completely obscured. At intermediate distances, objects are difficult but not impossible to discern. In the image above, the tree to the left corresponds to an optical depth of approximately 1, since it is mostly obscured, though still visible. The person in the foreground is at an optical depth of less than 1 (perhaps around 0.5), since they are easily discernable and there is very little fog blocking light between the person and the observer. Lastly, the end of the road is at an optical depth much greater than 1, since it is completely covered over by the fog and invisible to the observer.