通过比较旋转遮光带日射表(RSP)和参考标准表所测散射辐照度之间的数值差异,分析了太阳总辐照度、环境温度、相对湿度和太阳光谱等气象要素对RSP散射辐照度测量误差的影响关系,提出了一种修正RSP散射辐照度测量值的新算法。该算法从支...通过比较旋转遮光带日射表(RSP)和参考标准表所测散射辐照度之间的数值差异,分析了太阳总辐照度、环境温度、相对湿度和太阳光谱等气象要素对RSP散射辐照度测量误差的影响关系,提出了一种修正RSP散射辐照度测量值的新算法。该算法从支持向量机回归预测角度,建立了对RSP散射误差修正值的一次预测模型,然后根据误差修正值最优预测模型推导出RSP散射辐照度修正算法模型。利用该算法对美国国家太阳辐射研究实验室和劳里观测站采集的RSP散射辐照度数据进行修正,修正后两观测站数据的平均偏差和均方根误差分别降低到-0.2W/m2,3.3W/m2和1.9W/m2,8.5W/m2,显示算法具有良好的修正性能和适用性。该算法能够有效避免Vignola算法中存在的欠修正和Vignola and Augustyn(VA)算法中存在的过修正现象。展开更多
The present work analyzes the effect of aerosols on the evolution of the atmospheric boundary layer (ABL) over Shangdianzi in Beijing.A one-dimensional ABL model and a radiative transfer scheme are incorporated to dev...The present work analyzes the effect of aerosols on the evolution of the atmospheric boundary layer (ABL) over Shangdianzi in Beijing.A one-dimensional ABL model and a radiative transfer scheme are incorporated to develop the structure of the ABL.The diurnal variation of the atmospheric radiative budget,atmospheric heating rate,sensible and latent heat fluxes,surface and the 2 m air temperatures as well as the ABL height,and its perturbations due to the aerosols with different single-scattering albedo (SSA) are studied by comparing the aerosol-laden atmosphere to the clean atmosphere.The results show that the absorbing aerosols cause less reduction in surface evaporation relative to that by scatting aerosols,and both surface temperature and 2 m temperature decrease from the clean atmosphere to the aerosol-laden atmosphere.The greater the aerosol absorption,the more stable the surface layer.After 12:00 am,the 2 m temperature increases for strong absorption aerosols.In the meantime,there is a slight decrease in the 2 m temperature for purely scattering aerosols due to radiative cooling.The purely scattering aerosols decrease the ABL temperature and enhance the capping inversion,further reducing the ABL height.展开更多
文摘通过比较旋转遮光带日射表(RSP)和参考标准表所测散射辐照度之间的数值差异,分析了太阳总辐照度、环境温度、相对湿度和太阳光谱等气象要素对RSP散射辐照度测量误差的影响关系,提出了一种修正RSP散射辐照度测量值的新算法。该算法从支持向量机回归预测角度,建立了对RSP散射误差修正值的一次预测模型,然后根据误差修正值最优预测模型推导出RSP散射辐照度修正算法模型。利用该算法对美国国家太阳辐射研究实验室和劳里观测站采集的RSP散射辐照度数据进行修正,修正后两观测站数据的平均偏差和均方根误差分别降低到-0.2W/m2,3.3W/m2和1.9W/m2,8.5W/m2,显示算法具有良好的修正性能和适用性。该算法能够有效避免Vignola算法中存在的欠修正和Vignola and Augustyn(VA)算法中存在的过修正现象。
文摘The present work analyzes the effect of aerosols on the evolution of the atmospheric boundary layer (ABL) over Shangdianzi in Beijing.A one-dimensional ABL model and a radiative transfer scheme are incorporated to develop the structure of the ABL.The diurnal variation of the atmospheric radiative budget,atmospheric heating rate,sensible and latent heat fluxes,surface and the 2 m air temperatures as well as the ABL height,and its perturbations due to the aerosols with different single-scattering albedo (SSA) are studied by comparing the aerosol-laden atmosphere to the clean atmosphere.The results show that the absorbing aerosols cause less reduction in surface evaporation relative to that by scatting aerosols,and both surface temperature and 2 m temperature decrease from the clean atmosphere to the aerosol-laden atmosphere.The greater the aerosol absorption,the more stable the surface layer.After 12:00 am,the 2 m temperature increases for strong absorption aerosols.In the meantime,there is a slight decrease in the 2 m temperature for purely scattering aerosols due to radiative cooling.The purely scattering aerosols decrease the ABL temperature and enhance the capping inversion,further reducing the ABL height.
