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首页> 外文期刊>Atmospheric and oceanic science letters >Dust particles in free troposphere over Chinese desert region revealed from balloon borne measurements under calm weather conditions
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Dust particles in free troposphere over Chinese desert region revealed from balloon borne measurements under calm weather conditions

机译:平静天气条件下气球传播的测量结果揭示了中国沙漠地区对流层中的尘埃颗粒

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TThe Taklamakan Desert in China is one of the major source regions for Asian dust particles. All balloon-borne measurements in this report were carried out in Dunhuang, in the Taklamakan Desert, during calm weather conditions. The aerosol number concentration, size distribution, mass concentration, and horizontal mass flux due to westerly wind were investigated. The measurements were performed on 17 August 2001, 17 October 2001, 11 January 2002, and 30 April 2002. Five channels (0.3, 0.5, 0.8, 1.2, and 3.6?μm in diameter) were used in the Optical Particle Counter for particle measurements. The aerosol number concentration in the winter season (11 January 2002) at 3–5 km was very high. Variation of free-tropospheric aerosols on 30 April 2002 was noticeable. A super-micron range was noticeable in the size distribution of all the measurements. Many variations in temperature and aerosol concentration were found at these inversion points. High values of estimated mass concentration of aerosols were frequently observed in the atmosphere near the ground (i.e., 1–2 km); and interestingly, relatively high concentrations were frequently detected above 2 km from the surface. Wind patterns observed using ERA-Interim data at 500 and 850?hPa showed that westerly winds dominated in the Taklamakan Desert during the observation period. The average horizontal mass flux of background Asian dust due to westerly wind was observed to fall within the range of 58.5–1219 tons km~(?2) d~(?1). Vertical profiles of aerosol number concentrations showed that significant transport of aerosols dominated in the westerly region (i.e., 4–7 km).摘要塔克拉玛干沙漠是亚洲沙尘气溶胶的重要源地。为探讨塔克拉玛干地区沙尘气溶胶的理化特性与时空变化,研究其环境与气候效应,本文分析了四个季节在中国敦煌(塔克拉玛干沙漠内)取得的探空气球观测数据,包括气溶胶的数浓度、粒径分布、质量浓度及在西风主导下的水平输送通量。气溶胶数浓度的垂直廓线显示,来自沙漠地区的矿物粒子对局地环境与气候有重要影响,且所有季节都存在长距离输送。粒子谱分布显示局地有大量粗粒子输入。结果说明,源于塔克拉玛干沙漠的沙尘气溶胶的背景输送有着重要的科学意义,需进一步研究其对东亚和西太平洋地区环境与气候的影响。
机译:T中国的塔克拉玛干沙漠是亚洲尘埃颗粒的主要来源地区之一。本报告中的所有气球载测量均在天气平静的情况下在塔克拉玛干沙漠的敦煌进行。研究了西风引起的气溶胶浓度,粒径分布,质量浓度和水平通量。在2001年8月17日,2001年10月17日,2002年1月11日和2002年4月30日进行了测量。光学颗粒计数器使用了五个通道(直径分别为0.3、0.5、0.8、1.2和3.6?μm)进行颗粒测量。 。冬季(2002年1月11日)3-5 km处的气溶胶浓度非常高。 2002年4月30日对流层气溶胶的变化十分明显。在所有测量的尺寸分布中,超微米范围是明显的。在这些反转点发现温度和气溶胶浓度有许多变化。在地面附近(即1-2 km)的大气层中经常观察到较高的估计气溶胶质量浓度值;有趣的是,经常在距地面2 km以上的地方发现相对较高的浓度。使用ERA-Interim数据在500和850?hPa处观测到的风型表明,塔克拉玛干沙漠在观测期间以西风为主。观测到的西风背景亚洲粉尘的平均水平质量通量在58.5-1219吨km〜(?2)d〜(?1)范围内。垂直分布的气溶胶数量浓度表明,在西风区(即4-7 km)中,气溶胶的主要运移占主导地位。摘要塔克拉玛干沙漠是亚洲沙尘气溶胶的重要源地。为探讨塔克拉玛干地区沙尘气溶胶的理化特性与时空变化,研究其环境与气候效应,本文分析了四个季节在中国敦煌(塔克拉玛干沙漠内)获得的探空球观测数据,包括气溶胶的数密度,体积分布,质量浓度及在西风气体的数浓度的垂直轮廓线显示,来自沙漠地区的矿物粒子对局地环境与气候有重要影响,且所有季节都存在长距离输送。粒子谱分布显示局地有结果说明,源于塔克拉玛干沙漠的沙尘气溶胶的背景输送具有重要的科学意义,需要进一步研究其对东亚和西太平洋地区环境与气候的影响。

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