Estimation of aerosol single scattering albedo from solar direct spectral radiance and total broadband irradiances measured in China
نویسندگان
چکیده
[1] Aerosol single scattering albedo (wo) is a primary factor dictating aerosol radiative effect. Ground-based remote sensing of wo has been employed most widely using spectral sky radiance measurements made from a scanning Sun photometer. Reliable results can be achieved for high aerosol loadings and for solar zenith angle >50 . This study presents an alternative method using spectral direct radiance measurements or aerosol optical depths together with total sky irradiance to retrieve wo. The method does not require sky radiance data that can only be acquired by the expensive scanning Sun photometer. The method is evaluated using extensive measurements by a suite of instruments deployed in northern China under the East Asian Study of Tropospheric Aerosols: An International Regional Experiment (EAST-AIRE) project. The sensitivities of the retrieval to various uncertain factors were first examined by means of radiative transfer simulations. It was found the retrieval is most sensitive to cloud screening, total irradiance and the Angstrom Exponent (AE), but only weakly depends on surface albedo and the fine structure of aerosol size distribution. Using 1 year of rigorously screened clear-sky measurements made at the Xianghe site, the retrieved wo values were found to agree with those retrieved from the Cimel Sun photometer by the AERONET method to within 0.03 (RMS), and 0.003 (mean bias). As part of the differences originate from different sky views seen by the Sun photometers and pyranometer under comparison, a further test was conducted by using total sky irradiances simulated with the retrieved aerosol properties from the AERONET. The resulting estimates of wo agree to within 0.01–0.02 (RMS differences) and 0.002–0.003 (mean bias). These values are better measure of the true retrieval uncertainties, as they are free from any data mismatch. The characteristics of wo retrievals were discussed.
منابع مشابه
Comparison of UV-RSS spectral measurements and TUV model runs for clear skies for the May 2003 ARM aerosol intensive observation period
The first successful deployment of the fullyoperational ultraviolet rotating shadow-band spectroradiometer occurred during the May 2003 US Department of Energy’s Atmospheric Radiation Measurement program’s Aerosol Intensive Observation Period. The aerosol properties in the visible range were characterized using redundant measurements with several instruments to determine the column aerosol opti...
متن کاملUV spectral model and measurement comparisons
Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Abstract Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion EGU Abstract The first successful deployment of the fully-operational ultraviolet rotating shadow-band spectroradiometer occurred during the May 2003 U.S. Departmen...
متن کاملPhysical, chemical, and ultraviolet radiative characteristics of aerosol in central Alaska
[1] A new long-term monitoring site for providing multiwavelength (ultraviolet through near-infrared) and broadband irradiances has been established at the Poker Flat Research Range, Alaska, in order to assess the impacts of ozone, cloud cover, surface albedo, and aerosol conditions on trends in ultraviolet (UV) radiation reaching the surface. Targeted field measurements were conducted in the f...
متن کاملModelling and measuring the spectral bidirectional reflectance factor of snow-covered sea ice: an intercomparison study
Broadband albedo is a very important geophysical parameter in the Earth surface–atmosphere interaction in either global climate change or hydrological cycle and snowmelt runoff studies. To derive the broadband albedo accurately from satellite optical sensor observation at limited bands and at a single observation angle, the bidirectional reflectance factor (BRF) has to be specified quantitative...
متن کاملOn the Wavelength Dependence of the Absorption of Black Carbon Particles: Predictions and Results from the TARFOX Experiment and Implications for the Aerosol Single Scattering Albedo
We present measurements of the wavelength dependence of the aerosol absorption coefficient taken during the TARFOX experiment over the Northern Atlantic. The data show an approximate λ variation between 0.40 μm and 1.0 μm. We explore the theoretical basis of the wavelength variation of the absorption of solar radiation by elemental carbon (or black carbon, BC). For a wavelength independent refr...
متن کامل