Abstract
Abstract. This paper presents the reconstruction of the 80-year time series of daily global solar radiation (GSR) at the subtropical high-mountain Izaña Atmospheric Observatory (IZO) located in Tenerife (The Canary Islands, Spain). For this purpose, we combine GSR estimates from sunshine duration (SD) data using the Ångström–Prescott method over the 1933/1991 period, and GSR observations directly performed by pyranometers between 1992 and 2013. Since GSR measurements have been used as a reference, a strict quality control has been applied based on principles of physical limits and comparison with LibRadtran model. By comparing with high quality GSR measurements, the precision and consistency over time of GSR estimations from SD data have been successfully documented. We obtain an overall root mean square error (RMSE) of 9.2% and an agreement between the variances of GSR estimations and GSR measurements within 92%. Nonetheless, this agreement significantly increases when the GSR estimation is done considering different daily fractions of clear sky (FCS). In that case, RMSE is reduced by half, to about 4.5%, when considering percentages of FCS > 40% (~ 90% of days in the testing period). Furthermore, we prove that the GSR estimations can monitor the GSR anomalies in consistency with GSR measurements and, then, can be suitable for reconstructing solar radiation time series. The reconstructed IZO GSR time series between 1933 and 2013 confirms change points and periods of increases/decreases of solar radiation at Earth's surface observed at a global scale, such as the early brightening, dimming and brightening. This fact supports the consistency of the IZO GSR time series presented in this work, which may be a reference for solar radiation studies in the subtropical North Atlantic region.
Highlights
Solar radiation controls the energy radiative balance in the Earth and, our weather and climate
The global solar radiation (GSR) times series between 1933 and 2013 has been successfully reconstructed combining GSR estimates from sunshine duration (SD) measurements (1933/1991) using the Ångström–Prescott method and GSR observations performed by different pyranometers (1992/2013) at Izaña Atmospheric Observatory (IZO)
The SD measurements taken by Campbell–Stokes recorders (CS) between 1993 and 2000 have been validated against the LibRadtran model DSR simulations for cloudfree days
Summary
Solar radiation controls the energy radiative balance in the Earth and, our weather and climate. García et al.: Reconstruction of global solar radiation time series at Izaña station but some authors associate them with changes in global cloud cover, atmospheric aerosols content (natural or anthropogenic), and to the role of direct and indirect aerosol effects (Stanhill and Cohen, 2001; Ramanathan et al, 2001; Wild et al, 2005; Wild, 2009). The comparison of the aforementioned approaches conclude that the use of complex relations instead of the simple linear relation proposed by Ångström– Prescott does not significantly improve the GSR estimates (Almorox and Hontoria, 2004; Yorukoglu and Celik, 2006) In this context, the goal of this work is to reconstruct the GSR time series between 1933 and 2013 at the Izaña Atmospheric Observatory (IZO) by using the Ångström–Prescott method on SD measurements (1933/1991), and GSR observations performed by pyranometers (1992/2013). IZO provides atmospheric measurements representative of free troposphere conditions of the subtropical North Atlantic region due to the quasipermanent subsidence regime typical of the subtropical region (Cuevas et al, 2013; Gomez-Pelaez et al, 2013, and references therein)
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