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Aerosol's optical and physical characteristics and direct radiative forcing during a shamal dust storm, a case study

机译:气溶胶的光学和物理特性以及血液尘暴期间的直接辐射强迫,案例研究

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Dust aerosols are analyzed for their optical and physical properties during an episode of a dust storm that blew over Kuwait on 26 March 2003 when the military Operation Iraqi Freedom was in full swing. The intensity of the dust storm was such that it left a thick suspension of dust throughout the following day, 27 March. The synoptic sequence leading to the dust storm and the associated wind fields are discussed. Ground-based measurements of aerosol optical thickness reached 3.617 and 4.17 on 26 and 27 March respectively while the ?ngstrom coefficient, α870/440, dropped to ?0.0234 and ?0.0318. Particulate matter concentration of 10 μm diameter or less, PM_(10), peaked at 4800 μgm~(?3) during dust storm hours of 26 March. Moderate Resolution Imaging Spectroradiometer (MODIS) retrieved aerosol optical depth (AOD) by Deep Blue algorithm and Total Ozone Mapping Spectrometer (TOMS) aerosol index (AI) exhibited high values. Latitude-longitude maps of AOD and AI were used to deduce source regions of dust transport over Kuwait. The vertical profile of the dust layer was simulated using the SKIRON atmospheric model. Instantaneous net direct radiative forcing is calculated at top of atmosphere (TOA) and surface level. The thick dust layer of 26 March resulted in cooling the TOA by ?60Wm~(?2) and surface level by ?175Wm~(?2) for a surface albedo of 0.35. Slightly higher values were obtained for 27 March due to the increase in aerosol optical thickness. Radiative heating/cooling rates in the shortwave and longwave bands were also examined. Shortwave heating rate reached a maximum value of 2Kday~(?1) between 3 and 5 km, dropped to 1.5Kday~(?1) at 6 km and diminished at 8 km. Longwave radiation initially heated the lower atmosphere by a maximum value of 0.2Kday~(?1) at surface level, declined sharply at increasing altitude and diminished at 4 km. Above 4 km longwave radiation started to cool the atmosphere slightly reaching a maximum rate of ?0.1Kday~(?1) at 6 km.
机译:在2003年3月26日在2003年3月26日在伊拉克自由摇摆时,在2003年3月26日吹过科威特的尘埃风暴的一集中分析了尘埃气溶胶。尘埃风暴的强度使得在3月27日,它在第二天留下了厚厚的灰尘悬浮液。讨论了导致灰尘风暴和相关风场的偶极序列。在3月26日和2月26日达到3.617和4.17的地基测量分别达到3.617和4.17,而ngstrom系数,α870/ 440滴到?0.0234和?0.0318。颗粒物质浓度为10μm或更小,PM_(10),在3月26日的尘埃风暴小时内以4800μgm〜(α3)达到峰值。通过深蓝色算法和全臭氧映射光谱仪(TOMS)气溶胶指数(AI)的温度分辨率成像光谱辐射器(MODIS)检索气溶胶光学深度(AOD)呈现高值。 AOD和AI的纬度 - 经度映射用于推导科威特的粉尘传输源区。使用Skiron大气模型模拟灰尘层的垂直轮廓。瞬时净直接辐射强制在大气层(TOA)和表面级顶部计算。 3月26日厚的灰尘层导致通过Δ60WM〜(α2)和表面水平的TOA冷却α175WM〜(Δ2),用于0.35的表面反照孔。由于气溶胶光学厚度的增加,3月27日3月份获得了略高的值。还检查了短波和长波带中的辐射加热/冷却速率。短途加热速率达到最大值2kday〜(?1)在3到5公里之间,达到1.5公里〜(?1),距6公里,8公里减。龙波辐射最初将较低气氛加热到表面水平的最大值0.2kday〜(?1),在越来越高的海拔地下降并在4公里下减少。高于4公里的长波辐射开始冷却气氛略微达到最高速率?0.1kday〜(?1)在6公里处。

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