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Clear sky emissivity as a function of the zenith direction

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  • Awanou, Cossi Norbert

Abstract

Using the Bliss's theory [1] which assimilates the atmosphere as a column constituted of plane and parallel layers, the expression of the clear sky emissivity as a function of the zenithal direction is established. Other relations as the mean emissivity and the temperature of a part of the celestial vault are also established. The power emitted by some parts of the sky are calculated. Experiments have been conducted. This paper describes the study and presents the results.

Suggested Citation

  • Awanou, Cossi Norbert, 1998. "Clear sky emissivity as a function of the zenith direction," Renewable Energy, Elsevier, vol. 13(2), pages 227-248.
    • Handle: RePEc:eee:renene:v:13:y:1998:i:2:p:227-248
    DOI: 10.1016/S0960-1481(97)00070-0
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    References listed on IDEAS

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    1. Berger, X. & Bathiebo, J. & Kieno, F. & Awanou, C.N., 1992. "Clear sky radiation as a function of altitude," Renewable Energy, Elsevier, vol. 2(2), pages 139-157.
    2. Awanou, Cossi Norbert & Hazoume, Roger-Paul, 1997. "Study of natural condensation of atmospheric humidity," Renewable Energy, Elsevier, vol. 10(1), pages 19-34.
    3. Awanou, Cossi Norbert, 1991. "Study of heat exchange radiatively in 7–14 μm band," Renewable Energy, Elsevier, vol. 1(3), pages 335-344.
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    Cited by:

    1. Kounouhewa, Basile & Awanou, Cossi Norbert, 1999. "Evaluation of the amount of the atmospheric humidity condensed naturally," Renewable Energy, Elsevier, vol. 18(2), pages 223-247.
    2. Kruczek, Tadeusz, 2015. "Use of infrared camera in energy diagnostics of the objects placed in open air space in particular at non-isothermal sky," Energy, Elsevier, vol. 91(C), pages 35-47.

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