Abstract
Abstract. Downwelling surface shortwave flux (DSSF) is a key parameter to addressing many climate, meteorological, and solar energy issues. Under clear sky conditions, DSSF is particularly sensitive to the variability both in time and space of the aerosol load and chemical composition. Hitherto, this dependence has not been properly addressed by the Satellite Application Facility on Land Surface Analysis (LSA-SAF), which operationally disseminates instantaneous DSSF products over the continents since 2005 considering constant aerosol conditions. In the present study, an efficient method is proposed for DSSF retrieval that will overcome the limitations of the current LSA-SAF product. This method referred to as SIRAMix (Surface Incident Radiation estimation using Aerosol Mixtures) is based upon an accurate physical parameterization coupled with a radiative transfer-based look up table of aerosol properties. SIRAMix considers a tropospheric layer composed of several major aerosol species that are conveniently mixed to reproduce real aerosol conditions as best as possible. This feature of SIRAMix allows it to provide not only accurate estimates of global DSSF but also the direct and diffuse DSSF components, which are crucial radiative terms in many climatological applications. The implementation of SIRAMix is tested in the present article using atmospheric analyses from the European Center for Medium-Range Weather Forecasts (ECMWF). DSSF estimates provided by SIRAMix are compared against instantaneous DSSF measurements taken at several ground stations belonging to several radiation measurement networks. Results show an average root mean square error (RMSE) of 23.6, 59.1, and 44.9 W m−2 for global, direct, and diffuse DSSF, respectively. These scores decrease the average RMSE obtained for the current LSA-SAF product by 18.6%, which only provides global DSSF for the time being, and, to a lesser extent, for the state of the art in the matter of DSSF retrieval (RMSE decrease of 10.9, 6.5, and 19.1% for global, direct, and diffuse DSSF with regard to the McClear algorithm). The main limitation of the proposed approach is its high sensitivity to the quality of the ECMWF aerosol inputs, which is proved to be sufficiently accurate for reanalyses but not for forecast data. Given the proximity of DSSF retrieval to the modeling of the atmospheric direct effect, SIRAMix is also able to quantify the direct radiative forcing at the surface due to a given atmospheric component (e.g., gases or aerosols).
Highlights
Downwelling surface shortwave flux (DSSF) is defined as the irradiance in the solar spectrum reaching the Earth’s surface per unit of surface
A new approach referred to as SIRAMix is proposed in this article to estimate the instantaneous global, direct, and diffuse downwelling surface shortwave flux under clear sky conditions
The main novelty of SIRAMix compared to the current state of the art in DSSF retrieval is the consideration of an aerosol layer made of several aerosol species that are differently combined to reproduce any aerosol situation on Earth
Summary
Downwelling surface shortwave flux (DSSF) is defined as the irradiance in the solar spectrum reaching the Earth’s surface per unit of surface. Knowing the spatial distribution and temporal evolution of DSSF is essential for understanding climate processes at the surface/atmosphere interface. DSSF is directly related to the atmospheric radiative forcing at the surface (Bi et al, 2013) and to the field of solar energy and photovoltaic power plants (Yoshida et al, 2013). In the absence of clouds, DSSF is mainly driven by solar inclination, water vapor content, and atmospheric aerosols. The latter particles generally have opposite effects on the direct and diffuse radiative components that constitute
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