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Lidar detection of high concentrations of ozone and aerosol transported from northeastern Asia over Saga, Japan

机译:激光雷达探测从东北亚运送到日本佐贺市的高浓度臭氧和气溶胶

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摘要

To validate products of the Greenhouse gasesObserving SATellite (GOSAT), we observed vertical profiles of aerosols, thincirrus clouds, and tropospheric ozone with a mobile-lidar system thatconsisted of a two-wavelength (532 and 1064 nm) polarization lidar and atropospheric ozone differential absorption lidar (DIAL). We used theselidars to make continuous measurements over Saga (33.24° N,130.29° E) during 20–31 March 2015. High ozone and high aerosolconcentrations were observed almost simultaneously in the altitude range0.5–1.5 km from 03:00 to 20:00 Japan Standard Time (JST) on 22 March 2015. Themaximum ozone volume mixing ratio was ∼ 110 ppbv. The maximaof the aerosol extinction coefficient and optical depth at 532 nm were 1.2 km and 2.1, respectively. Backward trajectory analysis and thesimulations by the Model of Aerosol Species IN the Global AtmospheRe(MASINGAR) mk-2 and the Meteorological Research Institute Chemistry-ClimateModel, version 2 (MRI-CCM2), indicated that mineral dust particles from theGobi Desert and an air mass with high ozone and aerosol (mainly sulfate)concentrations that originated from the North China Plain could have beentransported over the measurement site within about 2 days. These highozone and aerosol concentrations impacted surface air quality substantiallyin the afternoon of 22 March 2015. After some modifications of its physicaland chemical parameters, MRI-CCM2 approximately reproduced the high ozonevolume mixing ratio. MASINGAR mk-2 successfully predicted high aerosolconcentrations, but the predicted peak aerosol optical thickness was aboutone-third of the observed value.
机译:为了验证温室气体观测卫星(GOSAT)的产品,我们使用由两个波长(532和1064 nm)的偏振激光雷达和对流层臭氧差分吸收组成的移动激光系统观察了气溶胶,薄卷云和对流层臭氧的垂直剖面激光雷达(DIAL)。在2015年3月20日至31日期间,我们使用这些激光雷达对佐贺(33.24°N,130.29°E)进行了连续测量。从03:00到20:0.5-1.5 km的高度范围内几乎同时观测到高臭氧和高气溶胶浓度: 00日本标准时间(JST)于2015年3月22日。最大臭氧体积混合比为110 ppbv。 532 nm处的气溶胶消光系数最大值和光学深度分别为1.2 km和2.1。向后轨迹分析和全球大气(MASINGAR)mk-2气溶胶物种模型和气象研究所化学气候模型第2版(MRI-CCM2)的模拟表明,戈壁沙漠中的矿物尘埃颗粒和空气团来自华北平原的高浓度臭氧和气溶胶(主要是硫酸盐)浓度可能在2天左右的时间内传输到了测量地点。这些高臭氧和气溶胶浓度在2015年3月22日下午大大影响了地面空气质量。在对其物理和化学参数进行一些修改之后,MRI-CCM2大致再现了高臭氧体积混合比。 MASINGAR mk-2成功地预测了较高的气溶胶浓度,但预测的峰值气溶胶光学厚度约为观测值的三分之一。

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