Delta Eddington
Term · Meteorology and atmospheric science · MLC-T-MET-004913
A two-stream approximation method used in atmospheric radiative transfer models to simplify calculations of scattering and absorption. It represents the highly forward-peaked scattering by aerosols and clouds with a Dirac delta function, while the remaining, more isotropic part of the scattering phase function is approximated by a simple two-term expansion. This approach provides an efficient way to model the transfer of solar radiation through the atmosphere, balancing computational cost and accuracy.
| Identifier | MLC-T-MET-004913 |
|---|---|
| Field | Meteorology and atmospheric science |
Record as JSON
{
"id": "MLC-T-MET-004913",
"term": "Delta Eddington",
"field": "Meteorology and atmospheric science",
"definition": "A two-stream approximation method used in atmospheric radiative transfer models to simplify calculations of scattering and absorption. It represents the highly forward-peaked scattering by aerosols and clouds with a Dirac delta function, while the remaining, more isotropic part of the scattering phase function is approximated by a simple two-term expansion. This approach provides an efficient way to model the transfer of solar radiation through the atmosphere, balancing computational cost and accuracy.",
"url": "https://mlchart.com/terminology/meteorology/delta-eddington/"
}
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