平流层气溶胶

  • 网络stratospheric aerosols
平流层气溶胶平流层气溶胶
  1. 大气臭氧、平流层气溶胶的监测与分析;

    Monitoring and analysis of atmospheric ozone and stratospheric aerosols ;

  2. 本世纪最大的一次平流层气溶胶事件

    A largest event of stratospheric aerosols in present century

  3. 平流层气溶胶浓度反常对于中国上空大气浑浊度的影响

    Effect of anomalous concentration of the stratospheric aerosol on the turbidity over China

  4. 温度对平流层气溶胶光学常数及辐射特性的影响平流层通信及相关技术

    The temperature changing influence of optical constants on radiative properties of stratospheric aerosols

  5. 用曙暮光时的天光光强反演平流层气溶胶散射系数廓线

    Retrieval of the Profile of Stratospheric Aerosols from the Intensity of Skylight During Twilight Periods

  6. 1984~2000年印度洋与中国地区上空对流层中上层及平流层气溶胶变化和输送特征

    Characteristics of change and transport of aerosols in the middle and upper troposphere and stratosphere over Indian Ocean and China in 1984-2000

  7. 在底层大气中处处存在的元素硫从一开始就被认为是平流层气溶胶的主要成分。

    Sulphur , a ubiquitous element in the lower atmosphere was identified from the outset as a predominant component in the stratospheric aerosol .

  8. 结果表明:天池火山喷发形成的平流层气溶胶可维持3年长的时间,并对到达地表的太阳辐射有非常明显的削弱。

    The numerical simulation results indicate that the stratospheric aerosol caused by that eruption may exist about 3 years and influence the solar radiation significantly .

  9. 本文基于对曙暮光问题的系列研究,提出一个用曙暮光时的光强观测资料反演平流层气溶胶垂直分布的方案。

    Based on a serial study on twilight problems , this paper proposes a scheme for retrieving the vertical distribution of stratospheric aerosols using the intensity observations during twilight periods .

  10. 对流层与平流层大气气溶胶微粒子的激光散射特性

    Laser Scattering Characteristics of Atmospheric Aerosol Particles in Troposphere and Stratosphere

  11. 平流层火山气溶胶对长波辐射的影响

    The effects of stratospheric volcanic aerosols on longwave radiation

  12. 从光波的衰减测量决定大气气溶胶的谱分布平流层火山气溶胶对长波辐射的影响

    Determination of the size distribution of atmospheric aerosols by means of measurement of optical attenuation the effects of stratospheric volcanic aerosols on longwave radiation

  13. 平流层火山灰气溶胶层对全球温度影响的敏感性研究

    Sensitivity study of the effect of stratospheric volcanic aerosol layer on the global temperature