资源环境科技发展态势分析平台

In this work, water vapor radiative effect (WVRE) is studied by means of the Santa Barbara's Disort Radiative Transfer (SBDART) model, fed with integrated water vapor (IWV) data from 20 ground-based GPS stations in Spain. Only IWV data recorded during cloud-free days (selected using daily insolation data) were used in this study. Typically, for SZA = 60.0 +/- 0.5 degrees WVRE values are around - 82 and - 66 Wm(-2) (first and third quartile), although it can reach up - 100 Wm(-2) or decrease to - 39 Wm(-2). A power dependence of WVRE on IWV and cosine of solar zenith angle (SZA) was found by an empirical fit. This relation is used to determine the water vapor radiative efficiency (WVEFF = partial derivative WVRE/partial derivative IWV). Obtained WVEFF values range from - 9 and 0 Wm(-2) mm(-1)(- 2.2 and 0% mm(-1) in relative terms). It is observed that WVEFF decreases as IWV increases, but also as SZA increases. On the other hand, when relative WVEFF is calculated from normalized WVRE, an increase of SZA results in an increase of relative WVEFF. Heating rates were also calculated, ranging from 0.2 Kday(-1) to 1.7 Kday(-1). WVRE was also calculated at top of atmosphere, where values ranged from 4 Wm(-2) to 37 Wm(-2).