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Influence of atmospheric ice nucleus concentrations on cold cloud radiant properties and cold cloud reflectivity changes in past years

机译:过去几年中大气冰核浓度对冷云辐射特性和冷云反射率变化的影响

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摘要

PAL satellite dataset which have long temporal span is used in the study. Relationship between cold cioud reflectivity and aerosol concentration in Beijing is analyzed as an example. From analysis, cold cloud reflectivity is found to be well correlated with aerosol optical depth. Meanwhile, it is retro-correlated with surface visibility. The results mean that cold cloud reflectivity is possibly influenced by ice nucleus concentration changes. Analysis about cold cloud reflectivity changes during the period 1982 - 1999 in Beijing shows that reflectivity increases in earlier years and decreases in later years. The data of cold cloud reflectivity in China show that reflectivity in some regions has changed. For the reason that cold cloud is very important in global climate system, those changes of cold cloud reflectivity can lead to climate changes finally.
机译:本研究使用时间跨度较长的PAL卫星数据集。以北京的冷反射率与气溶胶浓度的关系为例。通过分析,发现冷云的反射率与气溶胶光学深度密切相关。同时,它与表面可见度具有逆相关性。结果表明,冷云反射率可能受冰核浓度变化的影响。对北京1982年至1999年期间冷云反射率变化的分析表明,反射率在前几年增加而在后几年减少。中国冷云反射率的数据表明,某些地区的反射率发生了变化。由于冷云在全球气候系统中非常重要的原因,这些冷云反射率的变化最终会导致气候变化。

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