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|Title: ||An Iberian climatology of solar radiation obtained from WRF regional climate simulations for 1950–2010 period|
|Authors: ||Perdigão, João|
Soares, Pedro M.M.
Costa, Maria João
Dasari, Hari Prasad
|Keywords: ||WRF model|
Downward solar radiation
|Issue Date: ||Dec-2017|
|Citation: ||Perdigão, J., R. Salgado, C. Magarreiro, P. M. M. Soares, M. Costa, H. Prasad Dasari, 2017, An Iberian climatology of solar radiation obtained from WRF regional climate simulations for 1950–2010 period. Atmospheric Research. Volume 198, 1 December 2017, Pages 151-162. https://doi.org/10.1016/j.atmosres.2017.08.016.|
|Abstract: ||The mesoscale Weather Research and Forecasting (WRF) Model is used over the Iberian Peninsula to generate
60 years (1950–2010) of climate data, at 5 km resolution, in order to evaluate and characterize the incident
shortwave downward radiation at the surface (SW↓), in present climate.
The simulated values of SW↓ in the period 2000–2009 were compared with data measured in Spanish and
Portuguese meteorological stations before and a statistical BIAS correction was applied using data from Clouds
and the Earth's Radiant Energy System (CERES), on board four different satellites. The spatial and temporal
comparison between WRF results and observations show a good agreement for the analyzed period, although the
model overestimates observations. This overestimation has a mean normalized bias of about 7% after BIAS
correction (or 17% for original WRF output). Additionally, the present simulation was confronted against another
previously validated WRF simulation performed with different resolution and set of parametrizations,
showing comparable results. WRF adequately reproduces the observational features of SW↓ with correlation
coefficients above 0.8 in annual and seasonal basis.
60 years of simulated SW↓ over the Iberian Peninsula were produced, which showed annual mean values that
range from 130 W/m2, in the northern regions, to a maximum of around 230 W/m2 in the southeast of the
Iberian Peninsula (IP). SW↓ over IP shows a positive gradient from north to south and from west to east, with
local effects influenced by topography and distance to the coast.
The analysis of the simulated cloud fraction indicates that clear sky days are found in> 30% of the period at
the southern area of IP, particularly in the Algarve (Portugal) and Andalusia (Spain), and this value increases
significantly in the summer season for values above 80%.|
|Appears in Collections:||FIS - Publicações - Artigos em Revistas Internacionais Com Arbitragem Científica|
CGE - Publicações - Artigos em Revistas Internacionais Com Arbitragem Científica
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