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In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
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Related Experiment Video

Updated: Jun 16, 2026

In Situ Surface Temperature Measurement in a Conveyor Belt Furnace via Inline Infrared Thermography
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Published on: May 30, 2020

Transfer of infrared radiation through clouds.

P M Kuhn, H K Weickmann, M J Lojko

    Applied Optics
    |February 4, 2010
    PubMed
    Summary

    This study introduces a new radiative transfer model for cloud absorption, improving infrared cooling calculations. The model accurately predicts cloud radiative properties without assuming cloud thickness.

    Area of Science:

    • Atmospheric Science
    • Radiative Transfer
    • Cloud Physics

    Background:

    • Calculating radiative transfer and infrared cooling in clouds is complex.
    • Previous models often rely on assumptions about cloud thickness and opacity.

    Purpose of the Study:

    • To develop a radiative transfer model for cloud absorption based on observational data.
    • To improve the accuracy of infrared cooling calculations for various cloud types.

    Main Methods:

    • Developed a model using an observationally determined volume absorption coefficient (0.0005–0.0007 cm⁻¹).
    • The model accommodates clouds of varying transparency and opacity based on thickness and absorption.

    Main Results:

    • Achieved agreement within a standard deviation of 12.0 W m⁻² between model calculations and approximately 140 observations.

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    The Use of High-resolution Infrared Thermography (HRIT) for the Study of Ice Nucleation and Ice Propagation in Plants
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  • The model successfully predicted radiative transfer without assuming cloud blackness or thickness.
  • Conclusions:

    • The developed radiative transfer model offers a more flexible and accurate approach to cloud radiative property calculations.
    • This advancement aids in better understanding and modeling Earth's energy balance.