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首页> 外文期刊>ournal of the Meteorological Society of Japan >Estimation of Dry Deposition during Asian Dust Events in Spring of 2002
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Estimation of Dry Deposition during Asian Dust Events in Spring of 2002

机译:2002年春季亚洲沙尘事件期间的干沉降估算

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Dry deposition of Asian dust has been estimated during the intensive dust events in spring 2002 (Period I: 15-24 March 2002, Period II: 4-13 Apri1 2002) using the Asian dust aerosol model (ADAM). The emission module including log-normal distributions of particle size of different soil types of Gobi, Sand, Loess, and Mixed soil in the Asian dust source regions, has been used to calculate the amount of dry deposition. The dry deposition estimated by ADAM is compared with that calculated by using the optical particle counter (OPC) observed at Anmyeondo in Korea. The correlation between the modeled and the calculated dry deposition, is found to be 0.78 and 0.54 in Periods I and II, respectively. The dry deposition velocity depends on the particle size with a minimum value of 0.0272 cm s−1 and 0.0269 cm s−1 in the size range of 0.82-1.35 μm in diameter in Periods I and II, respectively. The averaged spectral distribution of dry deposition indicates that the larger particles are more contributed to the total dry deposition amount than the smaller particles due to the large deposition velocity oflarger particles. Consequently, the dry deposition rate is found to be higher in regions closer to the Asian dust source regions.The estimated total dry deposition amounts over the South Korea, North Korea and Japan are found to be about 558, 955, and 729 k ton, in Period I, respectively and about 240, 364, and 196 k ton, in Period II, respectively.
机译:使用亚洲粉尘气溶胶模型(ADAM),在2002年春季的强尘事件(时段I:2002年3月15日至24日,时段II:2002年4月4日至13日)中估计了亚洲尘埃的干沉降。排放模块包括亚洲粉尘源地区的戈壁,沙地,黄土和混合土的不同土壤类型的粒径的对数正态分布,已用于计算干沉降量。将通过ADAM估算的干沉降与使用在韩国Anmyeondo观察到的光学粒子计数器(OPC)计算的干沉降进行比较。在时期I和II中,模拟和计算的干沉降之间的相关性分别为0.78和0.54。 I期和II期的干沉降速度取决于粒径,其最小值分别为0.0272 cm s-1和0.0269 cm s-1,粒径范围为直径0.82-1.35μm。干法沉积的平均光谱分布表明,由于较大颗粒的沉积速度较大,较大的颗粒比较小的颗粒对总的干燥沉积量贡献更大。因此,在靠近亚洲尘埃源地区的地区,干沉降率较高。据估计,韩国,朝鲜和日本的干沉降总量约为558、955和729千吨,第一阶段分别为240吨,364吨和196千吨。

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