刘晶晶, 王国英, 徐梓翔, 刘芸, 王骏, 闫庆, 华灯鑫. 太阳光度计定标方法和西安地区气溶胶光学特征的研究[J]. 红外与激光工程, 2020, 49(6): 20190404. DOI: 10.3788/IRLA20190404
引用本文: 刘晶晶, 王国英, 徐梓翔, 刘芸, 王骏, 闫庆, 华灯鑫. 太阳光度计定标方法和西安地区气溶胶光学特征的研究[J]. 红外与激光工程, 2020, 49(6): 20190404. DOI: 10.3788/IRLA20190404
Liu Jingjing, Wang Guoying, Xu Zixiang, Liu Yun, Wang Jun, Yan Qing, Hua Dengxin. Study on calibration method of sky radiometer and aerosol optical properties in Xi'an region[J]. Infrared and Laser Engineering, 2020, 49(6): 20190404. DOI: 10.3788/IRLA20190404
Citation: Liu Jingjing, Wang Guoying, Xu Zixiang, Liu Yun, Wang Jun, Yan Qing, Hua Dengxin. Study on calibration method of sky radiometer and aerosol optical properties in Xi'an region[J]. Infrared and Laser Engineering, 2020, 49(6): 20190404. DOI: 10.3788/IRLA20190404

太阳光度计定标方法和西安地区气溶胶光学特征的研究

Study on calibration method of sky radiometer and aerosol optical properties in Xi'an region

  • 摘要: 利用西安理工大学2015~2018年的太阳光度计观测资料,在传统Langley法定标的基础上,利用期望平均法和拟合平均法获得了更为稳定的仪器定标系数,分析了西安地区气溶胶光学厚度和Ångström波长指数的变化特征。研究结果表明:(1)仅用Langley法对仪器进行定标带来的误差较大,引入期望平均法与拟合平均法后,得到的仪器定标值更合理,有效解决了Langley法定标值波动较大的问题;(2)西安地区气溶胶光学厚度日变化呈现5种特征:平稳型、上升型、下降型、凹型和凸型,其中平缓型出现频率最低(3.55%),凸型出现频率最高(34.25%);(3) 500 nm气溶胶光学厚度季节均值为0.60±0.36,0.59±0.33,0.62±0.40,0.68±0.36,呈春夏低、秋冬高的季节变化趋势。Ångström波长指数季节均值在夏季最大(1.06±0.33),春季最小(0.81±0.32)。

     

    Abstract: On the base of Langley method, a more reliable instrument calibration coefficient was obtained after the expected average and fitting average method were used, and the spatiotemporal characteristics of aerosol optical depth(AOD) and Ångström wavelength exponent were analyzed using observations of sky radiometer at Xi'an University of Technology from 2015 to 2018. Results revealed that: (1) Only the Langley method is used to calibrate the instrument. The error is large. After the introduction of the expected average method and the fitted average method, the instrument calibration value obtained is more reasonable, effectively solving the problem of large fluctuations in the legal value of the Langley legal calibration value; (2) the diurnal variation of aerosol optical depth has 5 types: flat type, ascending type, descending type, convex type, and concave type, respectively. The frequency of flat type is lowest, 3.55%, and concave type is highest, 34.25%; (3) the seasonal variation of aerosol optical depth at 550 nm wavelength showed spring and summer are lower, and autumn and winter are higher, with the average values: 0.60±0.36, 0.59±0.33, 0.62±0.40, 0.68±0.36, respectively. Moreover, Ångström wavelength exponent have a highest value in summer (1.06±0.33), and have a lowest value in spring (0.81±0.32).espectively. Moreover, Ångström wavelength exponent have a highest value in summer (1.06±0.33), and have a lowest value in spring (0.81±0.32).al variation of aerosol optical depth at 550 nm wavelength showed spring and summer are lower, and autumn and winter are higher, with the average values: 0.60±0.36, 0.59±0.33, 0.62±0.40, 0.68±0.36, respectively. Moreover, Ångström wavelength exponent have a highest value in summer (1.06±0.33), and have a lowest value in spring (0.81±0.32).

     

/

返回文章
返回