Bristow and Campbell model

A relationship between atmospheric transmittance and the daily range of air temperature is developed.This simple model can explain 70-90% of the daily solar radiation changes.

Air temperatureSolar radiationMathematical modelTempérature airRayonnement solaire

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Initial contribute: 2021-09-06

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  • KL Bristow
  • GS Campbell
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    Quoted from:[1] Bristow K L ,  Campbell G S . On the relationship between incoming solar radiation and daily maximum and minimum temperature[J]. Agric Forest Meteorol, 1984, 31(2):159-166.

    https://www.sci-hub.ren/10.1016/0168-1923(84)90017-0

    A relationship between atmospheric transmittance and the daily range of air temperature is developed. Tests on three data sets indicate that 70–90% of the variation in daily solar radiation can be accounted for by this simple model

     

    Bristow and Campbell developed a simple model for daily global solar radiation with a different structure in which H is an exponential function of Δ𝑇
    \( 𝐻/𝐻_0 =𝑎[1−exp⁡(−𝑏Δ𝑇^𝑐 )] \)
    where Δ𝑇 is the temperature term difference. Although coeffificients a, b and c are empirical, they have some physical meaning. Coeffificient a represents the maximum radiation that can be expected on a clear day. Coeffificients b and c control the rate at which a is approached as the temperature difference increases.

     

     

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    KL Bristow, GS Campbell (2021). Bristow and Campbell model, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/3c13f976-1c67-45e8-83dd-9bc92260eedc
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    Contributor(s)
    Initial contribute : 2021-09-06

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    Authorship

  • KL Bristow
  • GS Campbell
    • Is authorship not correct? Feed back

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