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  2. Atmospheric correction for interferometric synthetic aperture ...

    en.wikipedia.org/wiki/Atmospheric_correction_for...

    Freely available Global Atmospheric Models such as ERA5 data are generated using Copernicus Climate Change Service Information developed for numerical weather prediction. These models can provide accurate and high-resolution (still is coarse for InSAR studies) parameters for characterizing the atmosphere state.

  3. Mie scattering - Wikipedia

    en.wikipedia.org/wiki/Mie_scattering

    Like the Mie model, the extended model can be applied to spheres with a radius nearly the wavelength of the incident light. [36] The model has been implemented in C++ source code. [37] Recent developments are related to scattering by ellipsoid. [38] [39] [40] The contemporary studies go to well known research of Rayleigh. [41]

  4. Eady model - Wikipedia

    en.wikipedia.org/wiki/Eady_model

    First, the model assumes the atmosphere is composed of fluid obeying quasi-geostrophic motion. Second, the model assumes a constant Coriolis parameter. The model also assumes a constant static stability parameter and that fluctuations in the density of the air are small (obeys the Boussinesq approximation).

  5. ADMS 3 - Wikipedia

    en.wikipedia.org/wiki/ADMS_3

    The model is capable of simulating passive or buoyant continuous plumes as well as short duration puff releases. It characterizes the atmospheric turbulence by two parameters, the boundary layer depth and the Monin-Obukhov length, rather the single parameter Pasquill class. [2] ADMS 3 can simultaneously model up to 100 emission sources, of ...

  6. Mathematical model - Wikipedia

    en.wikipedia.org/wiki/Mathematical_model

    A mathematical model is an abstract description of a concrete system using mathematical concepts and language. ... including numerical instability. ...

  7. Upper-atmospheric models - Wikipedia

    en.wikipedia.org/wiki/Upper-atmospheric_models

    Whereas most climate models simulate a region of the Earth's atmosphere from the surface to the stratopause, [citation needed] there also exist numerical models which simulate the wind, temperature and composition of the Earth's tenuous upper atmosphere, from the mesosphere to the exosphere, including the ionosphere.

  8. Radiative transfer - Wikipedia

    en.wikipedia.org/wiki/Radiative_transfer

    Equations of radiative transfer have application in a wide variety of subjects including optics, astrophysics, atmospheric science, and remote sensing. Analytic solutions to the radiative transfer equation (RTE) exist for simple cases but for more realistic media, with complex multiple scattering effects, numerical methods are required.

  9. Category:Numerical climate and weather models - Wikipedia

    en.wikipedia.org/wiki/Category:Numerical_climate...

    Pages in category "Numerical climate and weather models" The following 102 pages are in this category, out of 102 total. ... Atmospheric model; Atmospheric Model ...