Surface Solar Radiation for Europe, Africa and the Atlantic based on MVIRI visible channnels

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Surface Solar Radiation for Europe, Africa and the Atlantic based on MVIRI visible channnels
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The EUMETSAT Satellite Application Facility on Climate Monitoring (CM SAF) provides a regional dataset of surface solar radiation, incoming direct radiation and effective cloud albedo at uniquely high spatial (0.03 deg) and temporal (up to hourly) resolutions for 1983 to 2005. The data set covers Europe, Africa, the Atlantic Ocean and parts of South America. Known as the CM SAF Surface Radiation MVIRI Data Set 1.0, the accuracy of a few W/M^2 (compared against BSRN) is comparable to or better than global products (such as NASA-GEWEX SRB). The data set is suitable for users seeking fine spatial and temporal resolutions for climate studies, evaluating global or regional models, or estimating potential solar energy production. The data are based on the visible channels of the METEOSAT Visible and Infrared Imager (MVIRI) on the Meteosat First Generation geostationary satellites.

Key Strengths

Key Strengths

Fine spatial and temporal resolutions and long record length

Useful for climate analyses and model evaluation, as well as estimating potential solar energy production

Accuracy well within range of comparable data sets (e.g. ISCCP; NASA-GEWEX SRB; Reanalyses)

Key Limitations

Key Limitations

only regional coverage

Please cite data sources, following the data providers' instructions
Suggested Data Citation
  1. Posselt, Rebekka; Müller, Richard; Stöckli, Reto; Trentmann, Jörg (2011): CM SAF Surface Radiation MVIRI Data Set 1.0 - Monthly Means / Daily Means / Hourly Means. Satellite Application Facility on Climate Monitoring. DOI:10.5676/EUM_SAF_CM/RAD_MVIRI/V001.

Hosted Climate Index Files
Usage Restrictions

Expert Developer Guidance

Expert Developer Guidance

#The following was contributed by Jörg Trentmann, (Eumetsat) February, 2013:

The CM SAF MVIRI surface radiation data set provides high-quality surface radiation data between 1983 and 2005 for the full disc of the Meteosat Geostationay Satellites, covering Europe, Africa and parts of South America, as well as the Atlantic Ocean. The data set includes the surface irradiance (i.e., global radiation), direct surface irradiance, and the effective cloud albedo. The data is provided as hourly, daily and monthy means on a regular lon-lat grid with a grid point distance of 0.03 deg. The high temporal and spatial resolution of the dats set is unique.

The data set has been validated against surface measurements of the irradiance and the direct irradiance from the Baseline Surface Radiation Network (BSRN). The accuracy of the monthly mean solar irradiance has been found to be approx. 8 W/m2, the accuracy of the corresponding direct solar radiation is approx. 11 W/m2. Further information of the validation results can be found in the validation report associated with the data set. Recent assessments of the temporal stability of the data set using surface reference observations from the Global Energy Balance Archive (GEBA) show a high stability in Europe after 1994.

The data set can be used to analyse the spatial distribution of surface solar radiation at local scales. The temporal and spatial resolution and the provision of the global and direct surface radiation allow the calculation of the potential of solar energy production. The high spatial resolution and the long time series allows the application of the data for climate model evaluation, incl. regional climate models. The stability of the data allows the detection and quantitfication of anomalies and the assessment of the temporal evolution incl. the determination of trends. The effective cloud albedo is a direct measure of the radiative effect of clouds on the top-of-the-atmosphere solar radiation and, hence, well suited for climate analysis.

In general, the validation with surface observations have shown that the data sets tends to overestimate the surface radiation by a few W/m2. The accuracy of the surface radiation is reduced over bright surfaces, due to the reduced effective cloud albedo. There are artificial 'stripes' and 'lines' in data before 1994 (only 'visible' at high spatial resolution) due to undocumented missing lines in the original satellite data. In general, the quality of the data decreases at high viewing angles, i.e., larger than approx. 60 deg, due to the overdetection of clouds at high viewing angles.##

Key Figures

Mean effective cloud albedo from 1994 to 2005 of the CM SAF Meteosat Surface Radiation data set. (Contributed by J. Trentmann)

Mean solar surface irradiance from 1994 to 2005 of the CM SAF Meteosat Surface Radiation data set. (Contributed by J. Trentmann)

Mean solar surface irradiance in July in Germany. Note the spatial variabilty induced by topographically-modified cloud coverage. (Contributed by J. Trentmann)

Time Series of the annual mean surface irradiance in Germany from 1983 to 2005. The years 1987/1998 and 2003 experienced the lowest / highest amount of solar irradiance. (Contributed by J. Trentmann)

Other Information

Earth system components and main variables
Type of data product
Dataset collections

Years of record
Data time period extended
No, data set not being extended
Sub-daily, Daily, Monthly
Input Data

Visible Satellite Channel, MVIRI instruments, Meteosat Satellites

Vertical Levels:
Missing Data Flag
Missing data present
Ocean or Land
Ocean & Land
Spatial Resolution

0.03 x 0.03 deg

Model Resolution (reanalysis)
Data Assimilation Method
Model Vintage (reanalysis)