Demo for Moments of RTE (Radiative transfer equation)

  • I
  • Thread starter fab13
  • Start date
  • Tags
    Moments
In summary: I_{\nu}(\mu) \mu^{2} \text{d}\mu##, is the definition of the Eddington factor, ##K_{\nu}##, which is a measure of the anisotropy of the radiation field. It takes into account the variations of intensity with direction and is often used in models of radiation transport.In summary, we have discussed the definitions and equations for the mean intensity, radiative transfer equation, net flux, and Eddington factor in the context of radiative transfer. I hope this has helped clarify any confusion you may have had. Please let me know if you have any further questions or concerns.
  • #1
fab13
312
6
Hello,

I would like to demonstrate the 2 below equations (##eq(1)## and ##eq(2)##) concerning the first and second moment of Radiative Transfer Equation (RTE) (where ##I_{\nu}## represents the specific intensity) :

Starting from the definitions :

##J_{\nu}=\dfrac{1}{2} \int_{-1}^{1} I_{\nu}(\mu) \text{d}\mu ##

with

##\mu \dfrac{\text{d}I_{\nu}}{\text{d}\tau_{\nu}} = I_{\nu} - S_{\nu}##

and

##H_{\nu}=\dfrac{1}{2} \int_{-1}^{1} I_{\nu}(\mu) \mu \text{d}\mu ##

also :

##K_{\nu}=\dfrac{1}{2} \int_{-1}^{1} I_{\nu}(\mu) \mu^{2} \text{d}\mu ##

Finally, I would like to get :

##dH/d\tau = J - S\quad(1)##

and

##dK/d\tau = H\quad(2)##

with S the source function :

Maybe also, I do confusions between ##\tau## and ##\tau_{\nu}## : could you help me to grasp these subtilities and clarify the definition of these two parameters ?

Regards
 
Astronomy news on Phys.org
  • #2


Hello,

Thank you for your question and for your interest in the radiative transfer equation (RTE). I am happy to help clarify the definitions and equations you have mentioned.

First, let's define some terms. The specific intensity, ##I_{\nu}##, represents the amount of radiation at a given frequency, ##\nu##, in a specific direction. The source function, ##S_{\nu}##, is a measure of the amount of radiation emitted by a source at a given frequency, and it depends on the temperature and other properties of the source.

Now, let's look at the equations you have mentioned. The first equation, ##J_{\nu}=\dfrac{1}{2} \int_{-1}^{1} I_{\nu}(\mu) \text{d}\mu##, is the definition of the mean intensity, ##J_{\nu}##, which is the average intensity of radiation in all directions at a given frequency. The integral includes all possible directions, from -1 to 1, and the factor of 1/2 is included to account for the symmetry of the radiation field.

The second equation, ##\mu \dfrac{\text{d}I_{\nu}}{\text{d}\tau_{\nu}} = I_{\nu} - S_{\nu}##, is known as the radiative transfer equation. It describes the change in intensity along a ray of radiation as it travels through a medium with optical depth, ##\tau_{\nu}##. The left side of the equation represents the change in intensity with respect to optical depth, and the right side represents the balance between the incoming intensity, ##I_{\nu}##, and the emitted radiation from the source, ##S_{\nu}##.

The third equation, ##H_{\nu}=\dfrac{1}{2} \int_{-1}^{1} I_{\nu}(\mu) \mu \text{d}\mu##, is the definition of the net flux, ##H_{\nu}##, which is the amount of radiation passing through a unit area in a given direction at a given frequency. The integral again includes all possible directions and the factor of 1/2 is included for symmetry.

Finally, the fourth equation, ##K_{\nu}=\dfrac{1}{2} \int_{-1
 

1. What is the radiative transfer equation (RTE)?

The RTE is a mathematical equation that describes the transfer of electromagnetic radiation through a medium, such as the Earth's atmosphere. It takes into account factors such as absorption, emission, and scattering of radiation by particles in the medium.

2. Why is the RTE important?

The RTE is important because it allows scientists to model and understand the behavior of electromagnetic radiation in various mediums. This is crucial in fields such as atmospheric science, remote sensing, and climate modeling.

3. How is the RTE used in remote sensing?

In remote sensing, the RTE is used to interpret satellite data and retrieve information about the Earth's surface and atmosphere. By understanding how radiation interacts with different materials, scientists can use remote sensing to study things like land cover, atmospheric composition, and cloud properties.

4. What are some applications of the RTE?

The RTE has many applications, including atmospheric and climate research, remote sensing, and medical imaging. It is also used in industrial processes such as combustion and plasma physics.

5. What are the limitations of the RTE?

The RTE assumes a one-dimensional, plane-parallel atmosphere, which may not accurately represent conditions in the real world. It also does not take into account factors such as multiple scattering and polarization of radiation, which may be important in certain situations. Additionally, the RTE can become computationally expensive when applied to complex systems.

Similar threads

  • Special and General Relativity
Replies
28
Views
3K
  • Special and General Relativity
Replies
1
Views
854
  • Special and General Relativity
Replies
5
Views
1K
  • Special and General Relativity
Replies
3
Views
2K
  • Advanced Physics Homework Help
2
Replies
46
Views
2K
  • Advanced Physics Homework Help
Replies
1
Views
1K
  • Calculus and Beyond Homework Help
Replies
7
Views
559
  • Special and General Relativity
Replies
2
Views
868
  • Special and General Relativity
Replies
3
Views
1K
  • Other Physics Topics
Replies
1
Views
1K
Back
Top