Renewable Energy Sources  
 

The irradiation varies with time of day but it can also vary considerably from location to location, especially in mountainous areas. Irradiation varies from an average of 1,000 kWh/m2 per year for northern European countries such as Germany, to 2,000 to 2,500 kWh/m2 per year for desert areas, as shown in Fig 2.1 for horizontal surfaces. These variations are caused by weather conditions and differences in the relative position of the sun (solar elevation) in the sky, which depends on the latitude of each location.

Although some benefit may be obtained by tilting solar panels to face the sun when it is not directly overhead, the improvement is less than might be expected under these conditions for two reasons:

· the atmosphere has already absorbed some energy due to the increased path length of solar rays through atmospheric dust and gases
· diffuse radiation from the rest of the sky partly compensates for this effect

Diffuse radiation also provides some energy on cloudy days, even though the sun may not be visible, and this is included in the data above.

 

2.3 Web Links

Interactive maps

The following websites are very useful for a view of the solar radiation in Europe depending on the period of the year.

 

1. Daily variation of sun shadows during several months:

· March: http://iamest.jrc.it/pvgis/pv/animations/images/eu_shadows_0321.gif
· June: http://iamest.jrc.it/pvgis/pv/animations/images/eu_shadows_0611.gif
· December: http://iamest.jrc.it/pvgis/pv/animations/images/eu_shadows_1221.gif

2. Monthly variation of global horizontal irradiation

http://iamest.jrc.it/pvgis/pv/animations/images/eu_globrad_year.gif

3. Daily variation of global horizontal irradiation

· December: htttp://iamest.jrc.it/pvgis/pv/animations/images/eu_globrad_1221.gif
· June: http://iamest.jrc.it/pvgis/pv/animations/images/eu_globrad_0621.gif

 

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