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Aerosol-cloud-precipitation effects over Germany as simulated by a convective-scale numerical weather prediction model

机译:对流尺度数值天气预报模型模拟的德国气溶胶-云降水效应

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pstrongAbstract./strong Possible aerosol-cloud-precipitation effects over Germany are investigated using the COSMO model in a convection-permitting configuration close to the operational COSMO-DE. Aerosol effects on clouds and precipitation are modeled by using an advanced two-moment microphysical parameterization taking into account aerosol assumptions for cloud condensation nuclei (CCN) as well as ice nuclei (IN). Simulations of three summer seasons have been performed with various aerosol assumptions, and are analysed regarding surface precipitation, cloud properties, and the indirect aerosol effect on near-surface temperature. We find that the CCN and IN assumptions have a strong effect on cloud properties, like condensate amounts of cloud water, snow and rain as well as on the glaciation of the clouds, but the effects on surface precipitation are a?? when averaged over space and time a?? small. This robustness can only be understood by the combined action of microphysical and dynamical processes. On one hand, this shows that clouds can be interpreted as a buffered system where significant changes to environmental parameters, like aerosols, have little effect on the resulting surface precipitation. On the other hand, this buffering is not active for the radiative effects of clouds, and the changes in cloud properties due to aerosol perturbations may have a significant effect on radiation and near-surface temperature./p.
机译:> >摘要。使用COSMO模型,在对流允许的配置中,接近于运行的COSMO-DE,研究了德国可能产生的气溶胶-云降水效应。考虑到云凝结核(CCN)和冰核(IN)的气溶胶假设,使用先进的两步微物理参数化对气溶胶对云和降水的影响进行建模。对三个夏季的模拟已在各种气溶胶假设下进行,并进行了有关表面降水,云性质和间接气溶胶对近地表温度的影响的分析。我们发现,CCN和IN假设对云的性质有很大影响,例如云水的凝结水量,雪和雨以及对云的冰川作用,但对表面降水的影响是?什么时候在空间和时间上平均?小。只有通过微物理过程和动力学过程的共同作用才能理解这种鲁棒性。一方面,这表明云可以解释为一种缓冲系统,其中环境参数(如气溶胶)的显着变化对最终的表面降水影响很小。另一方面,这种缓冲作用对云的辐射作用不起作用,并且由于气溶胶扰动而引起的云特性变化可能对辐射和近地表温度有显着影响。

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