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Radiation: Applications

The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
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Related Experiment Video

Updated: Jun 16, 2026

Construction of a Compact Low-Cost Radiation Shield for Air-Temperature Sensors in Ecological Field Studies
05:56

Construction of a Compact Low-Cost Radiation Shield for Air-Temperature Sensors in Ecological Field Studies

Published on: November 6, 2018

Differences in Radiance: relative effects of temperature changes and emissivity changes.

W L Wolfe

    Applied Optics
    |February 16, 2010
    PubMed
    Summary

    Changes in a material's emissivity significantly impact its radiance, comparable to temperature shifts. A small emissivity change of 0.01 is equivalent to a 0.5 K temperature variation in a 300 K environment.

    Area of Science:

    • Radiative transfer
    • Thermal physics
    • Remote sensing

    Background:

    • Understanding the interplay between temperature and emissivity is crucial for accurate radiance measurements.
    • Environmental factors like background radiation can influence observed radiance.
    • Quantifying the relative impact of these factors is essential for various applications.

    Purpose of the Study:

    • To calculate the relative effects of temperature and emissivity changes on radiance.
    • To analyze these effects for both total and monochromatic radiation.
    • To investigate the influence of different background conditions (none, uniform, nonuniform).

    Main Methods:

    • Radiative transfer calculations were performed.
    • Analysis considered total radiation and monochromatic radiation at peak contrast wavelength.

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    Construction of a Compact Low-Cost Radiation Shield for Air-Temperature Sensors in Ecological Field Studies
    05:56

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  • Simulations incorporated scenarios with no background, uniform background, and nonuniform background.
  • Main Results:

    • A change in emissivity of 0.01 corresponds to approximately a 0.5 K temperature change at a 300 K ambient.
    • This relationship holds true across different radiation types and background conditions.
    • Emissivity variations have a substantial effect on measured radiance.

    Conclusions:

    • Emissivity is a critical parameter in radiance calculations, with effects comparable to temperature changes.
    • Accurate emissivity data is vital for precise temperature retrievals in remote sensing and thermal analysis.
    • The study provides a quantitative basis for understanding these relative impacts under various conditions.