Overview
It is important to have advance knowledge on the incident solar irradiance in order to plan solar power plants and scale the heating infrastructure of buildings.
MeteoSwiss performs analyses of the spatial and temporal variability of the solar irradiance. The data used for such analyses accounts for the complex Alpine terrain and it includes the diverse interactions of horizon, snow cover and cloudiness in this terrain. The satellite climatology employed by MeteoSwiss consists of a multi-year dataset of solar irradiance derived from Meteosat Second Generation data back to 2004. It can be extended by Meteosat First Generation data back to 1983. The satellite climatology was validated with long term records of station data.
The potential yield of solar irradiance (kWh/m2) for Switzerland fo rthe period 2004-2009. The map was derived from Meteosat Second Generation satellite data with special emphasis on the complex interaction of topography, snow cover and cloudiness.
figure1_full.png, 1.9 MBWhat can be analyzed?
The seasonal and inter-annual variability of solar irradiance at a given location is needed in order to evaluate the suitability of a photovoltaic or thermal power plant or for calculating the energy consumption of a building. Satellite data of solar irradiance can further be used to create spatially distributed usability maps of solar irradiance. Depending on the application needs an extreme value analysis or an uncertainty estimation can be conducted.
Suitability map of the roof area for the city of St. Gallen. Red: highly suitable; orange: suitable; green: sufficient suitability; blue: unsuitable. Created by simuPlan for the City of St. Gallen by use of MeteoSwiss satellite-derived solar irradiance data.
figure2_full.png, 1.9 MBSolar energy data suitable for local town and country planning purposes is generally embedded in specific software tools used by engineers and city planners. Such software tools depend on the availability of spatio-temporally high resolution radiation components in order to calculate the energy balance of a geometrically complex infrastructure. Our analyses therefore include temporally fine grained time series of the most common solar radiation components used in solar energy applications.
Seasonal cycle (lines) and inter-annual variability (colored surfaces) of global radiation for Basel, Monte Rosa (Gorner Glacier, 3 km away from the Monte Rosa hut) and Klöntal (north face of the Glärnisch Mountain).
figure3_full.png, 195 KBWhat kind of data is used?
Our analyses are jointly based on spatially distributed satellite-derived solar irradiance maps and point-scale ground measurements. Ground measurements are very accurate for each respective measurement location, and satellite-derived solar irradiance maps allow analyses for regions without station coverage. The solar irradiance is not directly measured by satellite sensors. It is calculated by use of the so-called Heliosat algorithm. Through our long-term research collaboration within the EUMETSAT Satellite Application Facility on Climate Monitoring (CM SAF) the Heliosat algorithm was extended by MeteoSwiss. It is now suitable to calculate solar irradiance and radiation components in complex terrain and it for instance accounts for the reflective properties of snow. The resulting climatology was validataed with ground measurements. The satellite climatology can be de-biased with ground measurements if required by the application.
See Data Basis for more information.
Mean Direct Normal Irradiance (DNI, W m-2) for Europe during 2004-2010 calculated from Meteosat Second Generation satellite data.
figure4_full.png, 1.9 MBContact
Please contact us for further inquiries on solar energy analyses: klimainformation









