首页> 外文期刊>Environmental Monitoring and Assessment >POOL OF DUST PARTICLES OVER THE ASIAN CONTINENT: BALLOON-BORNE OPTICAL PARTICLE COUNTER AND GROUND-BASED LIDAR MEASUREMENTS AT DUNHUANG, CHINA
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POOL OF DUST PARTICLES OVER THE ASIAN CONTINENT: BALLOON-BORNE OPTICAL PARTICLE COUNTER AND GROUND-BASED LIDAR MEASUREMENTS AT DUNHUANG, CHINA

机译:亚洲大陆上的尘埃粒子池:中国敦煌的气球型光学粒子计数器和基于地面的激光测量

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摘要

Measurements of aerosols were made in 2001 and 2002 at Dunhuang (40°00'N, 94°30'E), China to understand the nature of atmospheric particles over the desert areas in the Asian continent. Balloon-borne measurements with an optical particle counter suggested that particle size and concentration had noticeable peaks in super micron size range not only in the boundary mixing layer but also in the free troposphere. Super-micron particle concentration largely decreased in the mid tropopause (from 5 to 10 km; above sea level, a.s.L). Lidar measurements made during August 2002 at Dunhuang suggested the possibility that mixing of dust particles occurred from near the ground to about 6km even under calm weather conditions, and a large depolarization ratio of paniculate matter was found in the aerosol layer. The top of the aerosol layer was found at heights of nearly 6km (a.s.l.). It is strongly suggested that nonspherical dust particles (Kosa particles) frequently diffused in the free atmosphere over the Taklamakan desert through small-scale turbulences and are possible sources of dust particles of weak Kosa events that have been identified in the free troposphere not only in spring but also in summer over Japanese archipelago. Electron microscopic experiments of the particles collected in the free troposphere confirmed that coarse and nonspherical particles observed by the mineral particle were major components of coarse mode (diameter larger than 1 μm) below about 5 km over Dunhuang, China.
机译:2001年和2002年在中国敦煌(北纬40°00',东经94°30')进行了气溶胶测量,以了解亚洲大陆沙漠地区大气颗粒的性质。用光学粒子计数器进行的气球式测量表明,粒径和浓度不仅在边界混合层而且在对流层中都在超微米尺寸范围内具有明显的峰值。在对流层顶中段(从5 km到10 km;高于海平面a.s.L),超微粒子浓度大大降低。 2002年8月在敦煌进行的激光雷达测量表明,即使在平静的天气条件下,尘埃颗粒也可能从地面附近混合到约6公里,并且在气溶胶层中发现了较大的去极化率。发现气溶胶层的顶部高度接近6 km(a.s.l.)。强烈建议非球形尘埃颗粒(科萨颗粒)经常通过小规模湍流在塔克拉玛干沙漠上方的自由大气中扩散,并且可能是在对流层中不仅在春季发现的弱科萨事件的尘埃颗粒来源而且夏天在日本群岛上空。对自由对流层中收集到的粒子的电子显微镜实验证实,由矿物粒子观测到的粗粒和非球形粒子是中国敦煌约5 km以下粗模式(直径大于1μm)的主要成分。

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