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The rate of heat transfer by emitted radiation is described by the Stefan-Boltzmann law of radiation:
Stokes' Law01:20

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Viscous forces, like friction, are intermolecular forces that resist the relative motion of molecules over each other. When a solid body moves through a liquid, viscous forces drag it in the opposite direction. The force's magnitude depends on the solid's shape and size, as well as its speed and the liquid's coefficient of viscosity, density and temperature.
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Radiation: Applications01:17

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Ostwald’s Dilution Law01:25

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Related Experiment Video

Updated: Jun 12, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Radiative transfer in stratified waters: a single-scattering approximation for irradiance.

W D Philpot

    Applied Optics
    |May 22, 2010
    PubMed
    Summary
    This summary is machine-generated.

    The singly scattered irradiance (SSI) model simplifies radiative transfer in shallow waters. This model aids in interpreting remote water color observations by implicitly including multiple scattering events.

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    Area of Science:

    • Ocean optics
    • Radiative transfer theory
    • Remote sensing

    Background:

    • Interpreting underwater light fields is crucial for remote sensing of water bodies.
    • Existing radiative transfer models can be complex for optically shallow waters.
    • The need for simplified yet accurate models for analyzing water color observations.

    Purpose of the Study:

    • To introduce and derive the singly scattered irradiance (SSI) model.
    • To provide a tool for interpreting remote sensing data of optically shallow stratified waters.
    • To offer a mathematically simple model that implicitly accounts for multiple scattering.

    Main Methods:

    • Derivation of the SSI model based on an analogy to single-scattering radiance models.
    • Implicit inclusion of multiple-scattering events by focusing on irradiance.
    • Expressing the model in terms of readily measurable parameters.

    Main Results:

    • The SSI model is presented as an approximate radiative transfer model.
    • The model's success depends on the near-independence of underwater radiance distribution from environmental factors.
    • Evidence supporting the qualitative and quantitative correctness of the SSI model is provided.

    Conclusions:

    • The SSI model offers a simplified approach to radiative transfer in shallow waters.
    • It effectively aids in the interpretation of remote water color observations.
    • The model balances mathematical simplicity with the retention of key radiative transfer subtleties.