首页> 外文期刊>Quarterly Journal of the Royal Meteorological Society >Physical and optical properties of mineral dust aerosol measured by aircraft during the GERBILS campaign. (Special Issue: Geostationary earth radiation budget intercomparison of longwave and shortwave radiation (GERBILS).)
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Physical and optical properties of mineral dust aerosol measured by aircraft during the GERBILS campaign. (Special Issue: Geostationary earth radiation budget intercomparison of longwave and shortwave radiation (GERBILS).)

机译:格柏斯战役期间飞机测量的矿物粉尘气溶胶的物理和光学特性。 (特刊:长波辐射和短波辐射的地球静止地球辐射预算比较(GERBILS)。)

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This paper presents aircraft measurements of the physical and optical properties of mineral dust from the GERBILS campaign. The campaign involved ten flights of the UK Facility for Airborne Atmospheric Measurements (FAAM) BAe-146 aircraft over the western region of the Sahara desert. Vertical profiles showed dust layers at varying altitudes extending as high as 6.5 km. Dust layers were typically associated with a deep well-mixed boundary layer or a residual boundary layer above (the Saharan air layer). Aerosol optical depths (AODs), measured by integrating vertical profiles of extinction coefficient, ranged from 0.3 to 2.4 (at 0.55 micro m). Aircraft AODs were generally within 20% of AERONET and Microtops sun-photometer measurements. Single-scattering albedos at 0.55 micro m were measured in the range 0.92-0.99 with a campaign mean of 0.97. The in situ size distribution compared well with AERONET retrievals made at Banizoumbou (Niger) and Dakar (Senegal). The proportion of aerosol volume associated with particles of radii >1.5 micro m was highly variable and also more difficult to measure. Models of dust as spheres, spheroids and more complex irregular-shaped particles were used to calculate single-scattering optical properties. The single-scattering albedo showed a low sensitivity to particle shape. The asymmetry parameter and specific extinction coefficient showed greater sensitivity to particle shape.
机译:本文介绍了GERBILS战役中矿物粉尘的物理和光学特性的飞机测量结果。该活动涉及英国机载大气测量设施(FAAM)BAe-146飞机在撒哈拉沙漠西部地区进行的十次飞行。垂直剖面显示,不同高度的尘埃层延伸高达6.5 km。灰尘层通常与深层充分混合的边界层或上方的残余边界层(撒哈拉空气层)相关。通过对消光系数的垂直剖面进行积分而测得的气溶胶光学深度(AOD)为0.3至2.4(在0.55微米处)。飞机的AOD通常在AERONET和Microtops太阳光度计测量值的20%以内。在0.92-0.99范围内测得0.55微米的单散射反照率,运动平均值为0.97。与在巴尼祖姆布(尼日尔)和达喀尔(塞内加尔)进行的AERONET检索相比,原位大小分布很好。与半径> 1.5微米的粒子相关的气溶胶体积比例变化很大,并且也更难测量。使用灰尘,球体和更复杂的不规则形状的颗粒模型来计算单散射光学特性。单散射反照率显示出对颗粒形状的低敏感性。不对称参数和比消光系数显示出对颗粒形状的更大敏感性。

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