fTemp: Intradaily evolution of ambient temperature
In solaR: Radiation and Photovoltaic Systems

Description Usage Arguments Details Value Author(s) References See Also

From the maximum and minimum daily values of ambient temperature, its evolution its calculated through a combination of cosine functions (ESRA method)

1	fTemp(sol, BD)

`sol`	A `Sol` object. It may be the result of the `calcSol` function.
`BD`	A `Meteo` object, as provided by the `readBD` function. It must include information about `TempMax` and `TempMin`.

The ESRA method estimates the dependence of the temperature on the time of the day (given as the local solar time) from only two inputs: minimum and maximum daily temperatures. It assumes that the temperature daily profile can be described using three piecewise cosine functions, dividing the day into three periods: from midnight to sunrise, from sunrise to the time of peak temperature (3 hours after midday), and to midnight.

A zoo object with the profile of the ambient temperature.

Oscar Perpiñán Lamigueiro.

Huld, T. , Suri, M., Dunlop, E. D., and Micale F., Estimating average daytime and daily temperature profiles within Europe, Environmental Modelling & Software 21 (2006) 1650-1661.
Perpiñán, O, Energía Solar Fotovoltaica, 2015. (https://oscarperpinan.github.io/esf/)
Perpiñán, O. (2012), "solaR: Solar Radiation and Photovoltaic Systems with R", Journal of Statistical Software, 50(9), 1-32, doi: 10.18637/jss.v050.i09

calcSol, readBD.

solaR documentation built on Oct. 19, 2021, 9:06 a.m.